Physical Geography - Rediscovering the Golden State https://rediscoveringthegoldenstate.com California Geography Fri, 24 Oct 2025 01:17:33 +0000 en-US hourly 1 https://wordpress.org/?v=6.9 149360253 Lonewolf Thunderhorse Captures Capricious Lightning https://rediscoveringthegoldenstate.com/lonewolf-thunderhorse-captures-capricious-lightning/?utm_source=rss&utm_medium=rss&utm_campaign=lonewolf-thunderhorse-captures-capricious-lightning Mon, 22 Sep 2025 18:27:11 +0000 https://rediscoveringthegoldenstate.com/?p=5129 It’s been revered, worshiped, and feared for centuries, thoroughly researched by stellar scientists, and altering landscapes across our state and around our world more than you might think. Because...

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It’s been revered, worshiped, and feared for centuries, thoroughly researched by stellar scientists, and altering landscapes across our state and around our world more than you might think. Because lightning accentuates many of the weather patterns covered in our previous website stories (such as our sporadic summer monsoon), we’re giving it more respect and attention here. This electrifying story was inspired by Oscar Rodriquez, AKA Lonewolf Thunderhorse. We will cap it with a haboob postscript that includes stunning videos.

Does Lightning Really Need an Introduction?

Lightning is anything but boring: volatile, explosive, cryptic, enigmatic, mystical, uncanny, fickle, erratic … pick your attribute. The National Severe Storms Laboratory has described lightning as a “capricious, random, stochastic and unpredictable event”. For thousands of years, people have marveled at these dazzling light shows that can be seen more than 100 miles away and their bombastic explosions of thunder that are propagated about a mile every 5 seconds and can be heard rumbling for more than 10 miles from the firebolt. Lightning has ignited fires that have incinerated ancient redwood forests and transformed nearly every other California plant community. If you explore the science behind lightning, you quickly understand how such shocking theatrics connect us and everything on our planet, always reminding us who’s boss.  

Southeast Arizona is often in the path of the first intrusions of summer monsoon air masses from Mexico. Frequent thunderstorms and their lightning displays decorate the sky well into September each year, when moisture from the south and east is injected into the desert heat. These clouds announce the arrival of mid- and high-level moisture. Add some sunlight and surface heating and you have the ingredients for afternoon thunderstorms that often rumble into the evening. This view looks over the Chiricahua Mountains. I recall being caught on a trail in this range one summer afternoon many years ago when a nearly clear sky quickly erupted into boiling cumulus clouds and a violent thunderstorm with frequent and dangerous cloud-to-ground lightning. Photo by Charles Hood.
You may not be able to see the top of cumulus clouds as they billow into icy glistening cumulonibus directly overhead. But when the bottoms of such budding thunderheads grow darker during summer afternoons in the southwestern US, it’s time to seek shelter. Cloud bases display the ascending air’s conndesation level and darker bottoms warn of thicker clouds with a lot more water. Starting here in eastern Arizona, the average frequency of summer storms deceases toward the west, until such clouds and Southwest Monsoon weather patterns become rare oddities along the California coast during summer. Photo by Charles Hood.  

Energy from the sun evaporates moisture, which rises and condenses into clouds, which releases latent heat, which fuels boiling thunderstorms, which helps to generate the awesome electric potential that sparks lightning. Typically, the tops of cumulonimbus clouds become positively charged, while negative charges accumulate on their bottoms. Though initial energy sources can also come from wildfires and volcanic eruptions, the most common trick is to get moist air to rise as fast as possible: the wettest and most unstable air masses generate the most severe thunderstorms with frequent lightning. Their narrow sparks of about 300 million volts or more can heat the air to 54,000°F (30,000°C), causing the explosive expansion of billions of air molecules and the crashing shock wave sound we know as thunder. As many as 2,000 thunderstorms are active on Earth at any time, totaling more than 14 million storms each year, generating about 6,000 lightning strikes each minute, and California experiences its share of these spectacles. Most lightning branches through the clouds, but when a cloud-to-ground bolt strikes too close, you will never forget it. I’ve seen trees splintered into shards and sandy soils melted and fused into glass-like branches (fulgurites) that trace the path of electric currents as they radiated out from where the bolts were first grounded.

You can see why I’ve used this photo in other stories about thunderstorms. This rogue storm drifted off the mountains and into the San Gabriel Valley during a rare extension of the monsoon far to the west, which eventually invaded SoCal’s highly populated coastal plains. You might notice the flat cloud bases near the center, marking condensation levels where updrafts are cooling to their dewpoints. Strong downdrafts driving heavy rain shafts are noticeable on each side. Photo by Matt Wright.  

It is true that tall objects, higher geographic features, and good conductors are most vulnerable, but erratic lightning can strike anywhere. Suffer a direct hit by a bolt, and you’re toast; but nearby strikes and distributary forks burn and electrocute more than 200 people in the US each year. Your chances of being struck are about 1/15,000 during your lifetime. And despite what you’ve heard, lightning originates in a cumulonimbus cloud and usually can travel only a few miles. (The record 500+ mile megaflash along a line of storms from Texas to Kansas City in 2017 is a very rare world-record exception. This AMS article is for you if you can’t get enough of the lightning science behind that shocking event.) Now that I’ve piqued your interest, I won’t repeat all the lightning details that are readily accessible elsewhere; you will find excellent links near the end of the next section of this story to guide you through the science, along with links to related stories on this website and narratives in my recent California Sky Watcher publication.

And Now, Introducing the Star of This Extreme Science Show

It’s time to return to the inspiration for this story: certified naturalist Oscar Rodriquez. Oscar writes how his creative name, Lonewolf Thunderhorse, “comes from my love of storms and wild nature—it captures the sense of being both solitary and deeply connected to the raw power of the earth and sky.” Perhaps that is why he happened to be in the right place at the right time, at The Commons in Chico, California on Tuesday, Aug. 26, 2025, around 9:30 p.m. Compared to previous years, California had experienced a relatively cool summer. But by late August, the weather patterns turned hot and turbulent. You can review the how-and-why details that led to such weather reversals (and their consequences) after Oscar shares his images and shocking storm experiences in his own words, from the Chico Commons.

A spectacular lightning display provided dramatic backdrop during this concert at The Commons in Chico on August 26, 2025. The thunderstorm drifted off the Sierra Nevada and the light show was captured by Oscar Rodriguez. 

The two shows started at 8 p.m. with the Wheeland Brothers, followed by Joe Samba. The music had the place buzzing when the storm moved in, making the night unforgettable. That day’s temperatures had climbed into the low 90s before cooling to the mid-70s after sunset. The heat mixed with lingering humidity set the stage for instability. Sure enough, a fast-moving storm built over the Sierra Nevada to the east and swept into the Sacramento Valley. By the time it hit Chico, it was alive with lightning—sharp forks that lit up the sky and turned the outdoor show into a dramatic showdown between music and nature. For the crowd, it was both exhilarating and dangerous—nature reminding us who was headliner.

In this video, Oscar’s camera focuses on the distant lightning rather than the blurred stage and band at Chico Commons. Here are L. Thunderhorse’s tech details:
Shot on my Samsung Galaxy S22, using Super Slow-Mo mode.
The fuzziness comes from the focus slipping in low light; unfortunately, I don’t have a clearer version.
The effect that looks like “linked snapshots” is just how Super Slow-Mo stitches frames together.
The round white dot you noticed on a lightning fork is an overexposure artifact—when the sensor is overwhelmed by lightning’s intensity, it creates that ghostly orb. Nothing was added or altered; the video is straight out of the camera.

Thanks again to my friend and former student Oscar Rodriguez for sharing his fortunate drama; he describes himself as a naturalist and “photographer and storm-chaser at heart”, which feels true to both the image and the story behind it.

This satellite image shows thunderstorms developing across western states several hours before Oscar captured the lightning. Some of the storms seen billowing over and east of the crest of the Sierra Nevada would eventually drift west toward Chico and the Sacramento Valley. The omnipresent marine layer’s stable low stratus and fog are visible off the coast. Source: National Weather Service.

The next section of this story follows those explosive air masses that invaded from the tropics into California during the end of our summer, 2025. When you have finished with our last sections, return here to these links for more lightning and thunderstorm science and details.

These sources help explain the science behind thunderstorms and the lightning they generate:

NOAA’s How Lightning is Created

Looking for More Details?

What Causes Thunder

Lightning Safety

Rare Sprites

The following links take you to previous stories on our website that feature thunderstorms:

Here are a few of our previous website stories following monsoon weather patterns:

Here are some of our previous stories highlighting lightning and wildfires:

Making Sense of the Monsoon Madness that Broke Summer’s Mildness

In contrast to recent summers, most of California experienced a cooler-than-average high-sun season into August, 2025. Persistent troughs of weak low pressure anchored along the west coast and spread cool sea breezes farther inland than usual; relatively dry, stable winds from the west pushed summer’s moist, muggy monsoon air masses far to the east or into Mexico. (Check out our previous website stories—listed above—about the Southwest/North American Monsoon.) But circulation patterns finally changed by mid-to-late-August, 2025, as summer’s familiar Four Corners High expanded over the desert southwest. Temperatures soared across the state, winds turned around the high pressure and swept summer storms into California from the southeast. Typical monsoon storms invaded inland California from Mexico and other southwest states until the steamy air masses were eventually blocked by our major mountain ranges; as is usually the case with our summer monsoon, folks west of the mountains (in cismontane California) could only look toward inland regions (transmontane California) to see distant towering cumulus and cumulonimbus clouds (AKA thunderheads).

By mid-August, 2025, the National Weather Service had already forecast a change in circulation patterns that would escort monsoon moisture into the southwest states. Note how this August 14 map illustrates how forecasters correctly anticipated the first substantial surge of monsoon moisture into inland California during the coming days. Also note how the green shaded areas of possible monsoon storms characteristically end along our major mountain barriers. In contrast, the wet and dry sides of California mountain barriers will switch when winter’s storms bring moisture directly off the Pacific to fall as orographic precipitation on west-facing slopes. Source: National Weather Service.   
On August 25, 2025, this 500mb chart shows upper-level pressure and wind patterns favorable for ushering monsoon moisture into transmontane California from the south and east. Oscar’s lightning images were captured on the next evening, as thunderstorms spilled out of the Sierra Nevada Mountains. Note the familiar location of the late summer Four Corners High. Source: National Centers for Environmental Prediction, Weather Prediction Center.   
These altocumulus cloud formations appeared to signal the first wave of monsoon moisture into California from the southeast.

The late arrival of heat and moisture glided north across the deserts, into the Basin and Range, and up along the spine of the Sierra Nevada Mountains, all the way into Oregon. Some storms brought beneficial rain to briefly interrupt summer’s drought, while other local storms generated that dreaded one-two-three punch so familiar with summer monsoon patterns: fierce dust storms (addressed in the Postscript of this story), dry lightning, and flash floods (see recent stories on our website). The heat and moisture brought instability and National Weather Service flash flood watches, which evolved locally to warnings across several states, into California. More than an inch of rain fell in an hour on desert locations from Yuma (on the AZ/CA/MX) border) into the Imperial Valley, nearly half their average annual total; the unstable moisture continued drifting north with steering winds, along and east of the Sierra Nevada spine and into northern Nevada.

Certain flight routes toward and out of LAX were briefly interrupted as jets couldn’t navigate around the big inland storms on Monday, August 28. Thousands of lightning strikes and up to 2 inches of rain in Sierra Nevada downpours (locally over 4 inches in Yosemite high country) generated sudden mudflows. Brief waterfalls were recorded over unlikely rock formations that included Lembert Dome above Tuolumne Meadows. In one week starting on August 22nd, California reported more than 74,000 lightning strikes. The flashes that danced over Chico (shared by Oscar in this story) came from one of these thunderstorms that spilled out of the Sierra Nevada and drifted over the Sacramento Valley.  

Residents of California’s coastal cities must usually look inland, toward the mountains, to watch summer monsoon storms develop. Scattered high and middle clouds in the foreground show us that plenty of moisture has been streaming in from the southeast. But distant mountains and intense afternoon heating in inland regions have lifted the moisture to condense and form towering cumulus and cumulonimbus clouds in the background. On very rare occasions, these storms might drift over the coastal plains.

Some of the storms delivered beneficial precipitation; others generated dangerous dry lightning that ignited more than 200 wildfires from the Sierra Nevada on up through the Klamath Mountains. Descriptive names were assigned to the big blazes, such as the Blue Fire and the SKU Late August Lightning Complex. But the Garnet Fire Complex stood out as it raged through Sierra National Forest east of Fresno and even threatened and burned below an ancient stand of giant sequoias. This article and video shows how the McKinley Grove was saved. Smoke from the Garnet Fire cut visibilities and spoiled air quality more than 100 miles away, depending on the wind currents, and it was still visible on satellite imagery into mid-September. 

The late August storm surge from the south even interrupted opening days at Burning Man when the spotty weather chaos barged across the Basin and Range to points north. This annual celebration of the bizarre (expecting nearly 70,000 people) was first disrupted by dust storms; thunderstorms followed with heavy rain and dangerous lightning across the exposed Black Rock Desert. Roads turning into the event were blocked and revelers who made it that far had long waits at closed entries as sudden downpours made thickening, gooey mud impassable and threatened visitors with electrocution. Severe thunderstorm warnings were issued again for the region (northern Washoe County) on Wednesday, August 26. During that last week of August, 2025, Black Rock lived up to its harsh high desert weather reputation, with temperatures ranging from the 90s during the hottest days to the 40s during the coldest nights, punctuated by fierce winds, dust storms, driving rainstorms, and wild variations in humidity ranging from the teens to over 90%.

This mudslide blocked a section of Interstate 80 east of Truckee near the California-Nevada border when an afternoon thunderstorm dumped heavy rain on Sierra Nevada slopes, August 27, 2025. (Caltrans Photo).

Across much of the American West, the relatively mild 2025 summer that started with a whimper was going out with a bang. Lonewolf Thunderhorse (featured earlier in this story) was lucky to capture a brief example of rare dramas orchestrated by nature when the western edge of summer’s Southwest Monsoon slops off the mountains and into California’s more densely populated inland valleys. 

Once the monsoon door was finally open in California, the on-and-off muggy thunderstorm drama acted out through mid-September. Steamy surges were augmented when the remains of Tropical Storm Mario were pulled up from the Baja coast on September 17, spreading rare storms into the coastal hills and plains. A few mountain locations received record rainfall (for specific dates) that totaled up to 4 inches, generating deadly and destructive flash floods and debris flows that cascaded down the mountains and raced through desert washes.

On this September 18, 2025 satellite photo, the remains of Tropical Storm Mario were circulating north and over California, spreading pockets of heavy rain. Source: National Weather Service.
By September 19, remnants of Tropical Storm Mario were drifting north past Southern California. But moist monsoon air masses (with dew points near 70°F) continued to keep showers in the forecast, even in coastal regions. Viewing beyond the pier, atypical low-level tropical moisture is lifted to form clouds over the Santa Monica Mountains. Farther inland, where heated air turned more unstable, severe thunderstorms and flash flooding caused havoc.   





 
 

A Postscript Celebrating Haboob Science

From northern Mexico and throughout the Desert Southwest, no discussion of summer thunderstorms is complete without acknowledging how they can generate some of the most bizarre weather events on Earth: haboobs. You don’t want to miss the breathtaking other-worldly haboob videos and the explanations that follow.  

It is important to recognize that all haboobs are dust storms but not all dust storms are haboobs. Haboobs may form when violent downdrafts fall out of thunderstorms. As these cold downbursts approach the ground, they become powerful outflow winds that often push ahead of the storms for many miles. Should you be engulfed by the blinding, choking wall of apocalyptic dust, remember the National Weather Service Slogan often echoed by transportation departments: Pull Aside, Stay Alive. 

As downbursts descend out of thunderstorms and into dryer air near the ground, melting ice and evaporating water cool the surrounding air parcels, causing them to plunge even faster. The powerful winds are then shoved ahead of the storm, kicking up thick walls of dust that can sweep across the landscape for many miles. A haboob is born. Source: Sciencenotes.org.

Here are some haboob videos and scientific explanations. (Please excuse any annoying advertisements in some of these videos: they’re not ours, but are imbedded within the links):

This unforgettable haboob video was filmed as the erratic monsoon surged through Arizona and spread toward California, one day before Oscar Rodriguez captured his Chico lightning in our story.

Another successful storm chaser shares her unforgettable haboob experience.

Here is video of the dust storm that ravaged Burning Man, 2025.

Various videos from Arizona and Burning Man as the same monsoon surged north.

Dust storm and haboob science explained:

https://www.youtube.com/watch?v=THSm-I790H0

https://dust.swclimatehub.info/2.3

https://www.noaa.gov/stories/haboobs-phenomena-with-unusual-name-is-no-joke

https://research.noaa.gov/how-deadly-are-dust-storms

More haboob science:

https://www.earthdate.org/episodes/dangerous-haboobs

A simpler haboob demonstration for the younger at heart:

Radar Characteristics of Dust Storms:

https://www.weather.gov/media/psr/Dust/2020/1_Rogers_Dust_Storm_Presentation_DustWorkshop2020.pdf

As autumn closes in, leaving another summer to fade away in our rearview mirrors, I am reminded of Bob Seger’s haunting lyrics that seem appropriate to end this stormy story:

I woke last night to the sound of thunder
How far off I sat and wondered …

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Geoengineering and Climate Intervention: Jet Trails and Radar and Cloud Seeding, Oh My! https://rediscoveringthegoldenstate.com/geoengineering-and-climate-intervention-jet-trails-and-radar-and-cloud-seeding-oh-my/?utm_source=rss&utm_medium=rss&utm_campaign=geoengineering-and-climate-intervention-jet-trails-and-radar-and-cloud-seeding-oh-my Wed, 16 Jul 2025 00:56:11 +0000 https://rediscoveringthegoldenstate.com/?p=5085 Our world is flooded with conflicting special interests pushing contradictory ideas and perspectives fueled by social media. So, you can’t blame folks for getting confused when trying to understand...

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Our world is flooded with conflicting special interests pushing contradictory ideas and perspectives fueled by social media. So, you can’t blame folks for getting confused when trying to understand some of the mysterious phenomena that surround us. Because it’s happened before and will likely happen again somewhere, it doesn’t take much imagination to suspect how secret government experiments might be impacting our environment and health. But just as it is our responsibility to keep governments and other powerful entities accountable, it is also our obligation to distinguish the difference between fact and fiction, casting aside the imagined so that we can focus on real issues and problems. This story will use critical thinking and the scientific method to help clear up some popular misconceptions about what has been popularly called geoengineering, AKA climate intervention or modification.

Contrails form and merge with ice-crystal cirrus in a nearly saturated atmosphere above around 25,000 feet. This is looking over Bolsa Chica Wetlands near Sunset Beach at sunset.

Geoengineering Cultures and Confirmation Bias

We can start with more than a decade of very public statements and events that finally inspired this story. My first big wakeup call came around 2011, while wandering into one of those Occupy Wall Street encampments at City Hall; I noticed a giant “Chemtrails=Geoengineering=Crimes Against Humanity” banner draped across the plaza. When I extended my hand and politely quizzed the protagonist about his sign, he asked me why I was bothering to explain the science for him and then he walked away in frustration. While radio-channel surfing several years ago, I chanced upon a DJ on a famously progressive-leaning all-news station asking for donations during a pledge drive. She was ranting about how chemtrails were so prevalent one day and absent on others, proving that some sort of secret government program was responsible for spraying our skies with poisonous chemicals that were changing our weather and how their investigative reporters were getting to the bottom of it all. Then there was the popular local TV news anchor who went on a special assignment interviewing people who believed that their health problems only flared up when those mysterious chemtrails appeared overhead above 25,000 feet. That perspective earned a series of prime-time TV stories shamelessly designed to boost network ratings.

The guy who was responsible for this banner was in no mood to talk about the science.

More recently, on May 15, 2025, I stumbled upon a popular right-leaning radio talk show interview with the documentary-maker, chemtrail promoter, and champion of climate conspiracy theories, Matt Landman. He trumpeted to millions of listeners how recent devasting fires in Hawaii and California (and other tragic disasters) were caused by geoengineering. He also claimed that rainmaking had been “perfected”, and all that government and other “powers that be” had to do is flip a switch and make it rain on top of those fires and put them out. I was finally pushed into doing this story when a friend of mine, who is educated about these matters, wrote, “I know several people including some smart friends who 100% believe jet trails are a nefarious something that is being done by the “government”. They say if the jet trails were just vapor, they would disappear right away and they don’t.”

Students in my field class admire strings of contrails (more than 20,000 feet above) from the top of the Santa Monica Mountains.

Regardless of your politics (geoengineering believers are commonly found on the far right and far left of the political spectrum) … Mission Control, we have a big information problem that needs our attention. Objective scientific explanations and analyses of climate intervention makes a lot of people uncomfortable; presenting solid evidence that unveils mysteries and may challenge true believers can foster resentment. Scientists and educators are sometimes intimidated until they become uneasy about truth-telling in such a hyped-up confirmation bias cancel culture. So, we must jump into this pop-culture controversy with our continuing commitment to just keep to the facts.

Jet Trails or Contrails or Chemtrails?

People have noticed and photographed jet trails (or contrails) in the sky for a century, ever since the beginning of jet aviation. In my book, The California Sky Watcher, I wrote about the science behind contrails in the section about clouds. Here is an excerpt with some editing for this story:

When you see jet trails—or condensation trails (contrails)—forming, they are announcing that the upper altitudes, where jets are flying, are near their dew points. You might notice them during any season, but once they form, they are likely to drift faster with higher-velocity winds as nature’s winter jet streams sweep farther south. Jets emit particulates and moisture from their exhaust into air at around 30,000 feet (9,140 m) altitude. Way up there, where it may be colder than –50°F (–46°C), vapor will almost immediately freeze around the jet exhaust to form ice-crystal cirrus-cloud streaks. When jet trails are thicker and last longer, there are often cirrus clouds forming near them in the saturated air at these high altitudes. When drier upper layers are not near their dew points, the jet trails will quickly sublimate (turn from ice directly into vapor) and disappear into the clear air. Jet trails may also quickly form by a process called aerodynamic condensation, which occurs as air is forced over the wings, causing adiabatic expansion and cooling of the moist air to its dew point. If you want to learn the detailed physics behind that specific process, here’s an article.

Technologies (see below) allow us to track particular airline flights that might be making trails; just follow their flight patterns. Research has shown that these slender clouds can combine to block and reflect enough shortwave sunlight back to space to suppress afternoon surface temperatures downward by a degree or more. When conditions are favorable, look for the linear shadows they can cast through hazy skies. But they also absorb longwave radiation from Earth’s surface at night, only to reradiate it back toward the surface, keeping overnight low temperatures just a bit warmer. The net result might be slight global warming in our atmosphere. At these high altitudes, the suspended jet exhaust pollution will likely be carried hundreds or thousands of miles in strong upper-level winds until it gets diluted and dispersed into global circulation patterns.

Contrails appeared to be mimicking the trend of granitic rock formations and topography here in Joshua Tree National Park. 

You might recognize how foolish it would be to attempt to poison a particular place or population with a chemtrail above 25,000 feet that is likely to drift a continent or ocean away as it is mixing and dispersing in the upper atmosphere. And then there are the thousands of scientists, engineers, pilots, and all the support staff and other workers who would be keeping these secrets from all of us. And don’t take my word or it. Check out the following explanations from the experts who dedicate their careers to researching this stuff.

Chem trails debunked: Royal Aeronautical Society

American Meteorological Society, 2017 Research Paper on Contrails

You can also use several apps (Flightradar24 , FlightAware , Plane Finder) that allow you to track flights in real-time and see exactly what planes are flying overhead. Flightradar24 even offers an augmented reality (AR) feature to identify planes by pointing your device at the sky. 

Some who have finally cast aside their claims of secret government flight chemtrails still argue that someone is purposely placing chemicals, designed to poison us and/or change the climate, into jet fuels. But fuels must be carefully formulated to keep flights safe and efficient and the dangerous chemicals often mentioned aren’t even found in jet fuels. Nevertheless, public officials, including our current US Health and Human Services Secretary, have fueled these rumors with reckless rhetoric and empty promises.

Some political leaders (from at least 8 states) are even trying to pass legislation to stop something that doesn’t exist. Here is an article that traces the roots of several decades of geoengineering history and some myths that have often been championed by those on the far left and then far right of the political spectrum, which is now morphing into legislation of the bizarre.

Viewing across the mountains, you can see a low layer of moist haze in the distance. A few cirrostratus clouds appear high above the otherwise clear air columns, announcing that upper levels are humid and ripe for formation of contrails behind passing jets.

Weather Radar

Another rumor gone viral (and promoted by some who must know better) is how weather radar stations are designed to change our weather. But radar technologies have been widely used in law enforcement and air traffic control and our atmosphere has always been bombarded with radio waves from the universe, not to mention more than a century of humans’ radio and TV waves. Equipment within “those round domes” you might see uses Doppler radar (microwaves on the electromagnetic spectrum) to detect the speed and direction of moving objects. They use the Doppler effect, tracking the change in frequency of their propagated and then reflected radio waves, to measure the direction and speed of objects in the sky. Those spherical “radomes” are just shells designed to shield the sensitive equipment inside and minimize interference with radar signals.

This “radome” in the Laguna Mountains protects sensitive equipment and minimizes interference. Radar technologies have become essential tools for tracking precipitation and storms.

These radar technologies have greatly improved forecasters’ ability to immediately monitor precipitation and storms as they form and move and they can even detect powerful winds and circulations in the clouds before they become dangerous funnel clouds or deadly tornadoes. You can thank such technologies for saving thousands of lives each year and making your plane flights safer. Yet, in the spirit of you can’t make this stuff up, some clueless (or worse) public officials have proposed banning them! Here’s another plea to not take my word for it and do your own research. How radar works

Weather radar stations in the US, including both NEXRAD (Next-Generation Radar) and TDWR (Terminal Doppler Weather Radar), are operated by different federal agencies. The National Weather Service (NWS), an agency within NOAA (National Oceanic and Atmospheric Administration), operates and maintains NEXRAD stations. The Federal Aviation Administration (FAA) maintains and operates TDWR stations. Additionally, the US Air Force also plays a role in the NEXRAD system.

You may also have heard the sordid stories about HAARP, especially from talk radio programs and other media looking to boost their ratings. This acronym for the scientific research facility in Alaska stands for High-frequency Active Auroral Research Program, where they have been using a high-frequency transmitter to study the ionosphere, that charged-up rarified top or our atmosphere that affects radio wave propagation and extends from more than 30 miles high on out into space. Unfortunately, HAARP research scientists have been accused of manipulating weather and even engaging in mind control, which should make us wonder who’s trying to control whom.

Cloud Seeding

Here’s where humans have been experimenting with weather modification for years, but with mixed results at best. So that we don’t try to reinvent the wheel, I will use another edited excerpt from my California Sky Watcher book to summarize cloud seeding in California:

“Cloud seeding is one of the most studied and debated forms of weather modification. It exploits natural processes to enhance precipitation from thick clouds that are potential precipitation producers. Such cloud-seeding experiments date back more than seventy years, with some “success.” Remember that most of the substantial rain you have experienced in California started high in the clouds as ice and snow that eventually melted before reaching the ground. In some clouds with favorable dynamics, adding just the right number of minute particles (either launched from the ground or from planes) that can act as freezing nuclei (such as silver iodide) seems to slightly enhance precipitation totals. This happens as the freezing nuclei grow layers of ice by attracting very cold water in clouds that then freezes on to the nuclei surfaces. (This is also known as the Bergeron process.) The ice crystals grow large enough to fall through the clouds, attracting more moisture along the way and producing heavier precipitation than might have been expected. (Similar methods have been used to clear thick, cold fog banks.) This process does not work in warm clouds that may drop lighter rain and drizzle.

Cloud seeding has had mixed results, but the process must begin with clouds that are at least potential precipitation producers. Silver iodide (an efficient ice nucleating agent) is usually the preferred additive. There’s nothing secret about these efforts; such images are available to all online.

Rain- and snowmaking is a tricky business given that even when seeding is considered successful, a lot of uncertainty and risk management remains. We have much more to learn about weather modification, which explains why the American Meteorological Society encourages only the most well-designed experimentation and research and recommends caution when people are fooling around with these natural processes. In spite of these uncertainties, as of 2025, several California agencies continued experimenting with cloud-seeding efforts, especially to enhance Sierra Nevada snowpacks. (An increasing number of studies have suggested snowfall enhancement success of up to 3–10 percent in the mountains.) Water and utility districts such as in Sacramento and the East Bay, PG&E, the Santa Ana Watershed Project Authority, and Santa Barbara and San Luis Obispo Counties continue their experimental programs, hoping for the best.

We have come a long way since Charles Hatfield roamed our drought-stricken state in the early 1900s, advancing what some believed to be his magical rainmaking skills. When he was finally hired to break the 1915 drought in San Diego, by chance a historic nearly 30 inches (76 cm) of rain fell in less than a month, causing devastating and deadly flooding. Hatfield’s shenanigans even inspired a classic 1950s Western movie, The Rainmaker. Our weather knowledge then was barely a drop in the bucket compared to what we know today, as better-informed scientists and would-be rainmakers continue with their weather modification debates and efforts. Such struggles with nature make me suspect that the Native Americans before us better understood some of California’s weather and water cycles.”

The historic July 4, 2025 flash flood tragedy along the Guadalupe River in Texas (see our adjacent website story) brought cloud seeding into the headlines again when it was learned how a California-based company called “Rainmaker” had been working in Texas. But the company had only seeded two small clouds in distant south-central Texas two days before the flood, and the puffy potential rainmakers evaporated within a couple of hours. Rainmaker wisely suspended operations two days before the Texas floods as moist air masses moved toward the region and forecast models warned of big storms in the days ahead. Still, clueless social media posts pointed fingers in attempts to displace the blame.

You will find a wealth of links to research on cloud seeding at the end of this story (below).

On this autumn day, some contrails seemed to form parallel to these barbed-wire fences and distant power lines east of the Sierra Nevada.

Become Part of the Solution by Spreading the Knowledge

It is our responsibility to combat confirmation bias by moving forward with transparency and integrity. Please share these back-to-reality facts with your friends who have been misled by some skeptics who are well-intentioned, some who are true believers and followers, some who take advantage of people’s fears and vulnerabilities, and others who should know better. Show them how old-fashioned critical thinking and use of the scientific method can clear up any confusion they might have about climate intervention/modification, or what they call geoengineering. And if they insist on following these distracting conspiracy theory trails that lead to dead ends, remind them of the old adage I have slightly modified, but applies perfectly here: “Fool me once, shame on you. Fool me twice, weird weather we’re having, eh?”

To repeat “Don’t take my word for it.”, here are some relevant links to share:

The Latest AMS Statement on Climate Intervention

NOAA Fact Check on Climate Modification

Weather Modification Project Reports from NOAA

Cloud Seeding Links and Details:

Recent GAO paper on Cloud Seeding

In case you missed that Texas flash flood/cloud seeding article, here’s the link sent from climatologist Bill Patzert.

From 2016: The California Department of Water Resources (DWR) has been regulating and monitoring cloud seeding programs in California, which are used to enhance precipitation, particularly snow and rain. These programs involve the release of substances like silver iodide into clouds to promote ice crystal formation and increase precipitation. The DWR requires sponsors to file notices of intent and comply with environmental regulations.

To track cloud seeding programs in the US, you can consult resources that include the Colorado Virtual LibraryNOAA’s Library, and the North American Weather Modification Council. Some other states also have their own programs, such as Colorado’s Weather Modification Program. Additionally, organizations such as the Desert Research Institute conduct research and operate cloud seeding projects.

Just in case you haven’t seen enough contrail images ….

Thin layers of cirrostratus clouds form in the saturated air more than 25,000 feet above the stadium light towers. Jets and their contrails join the ice party.
Streaks of high ice-crystal cirrus clouds stream ahead of an approaching warm front. Moistening upper layers set the stage for contrails to add some streaks as jets pass through.
Fall colors, cirrostratus clouds, and contrails decorate this autumn scene over Topaz Lake on the California/Nevada Border.
You may have noticed this home on the range below the jet trails scene in a previous story. We are looking west, toward distant Sierra Nevada high country.
Weathering granitic rocks at Joshua Tree National Park point toward crisscrossing contrails.
A lone bird flies far below contrails forming within a layer of wispy cirrostratus just after sunset. We can use the relatively stationary moon above to measure how these ice crystal cirrus are streaming fast across the winter sky. Because they are so far away, up to five miles high, you might not sense that they were drifting with upper-level winds at more than 100 mph.

THE END

The post Geoengineering and Climate Intervention: Jet Trails and Radar and Cloud Seeding, Oh My! first appeared on Rediscovering the Golden State.

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Flash Flood! … From Texas to California https://rediscoveringthegoldenstate.com/flash-flood-from-texas-to-california/?utm_source=rss&utm_medium=rss&utm_campaign=flash-flood-from-texas-to-california https://rediscoveringthegoldenstate.com/flash-flood-from-texas-to-california/#comments Tue, 15 Jul 2025 19:20:29 +0000 https://rediscoveringthegoldenstate.com/?p=5065 As the death toll rises to more than 130 and scores are still missing in the July 4, 2025 Texas flash flood, at least three questions haunt us: Why...

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As the death toll rises to more than 130 and scores are still missing in the July 4, 2025 Texas flash flood, at least three questions haunt us: Why did this happen, how could it have been prevented, and could it happen in California?

Made for Flash Floods

Some basic knowledge of the region’s geography and weather patterns helps us answer the first question. Headwaters of the Guadalupe River Basin are perfectly positioned in a region already known as “Flash Flood Ally”, within a sprawling swath across central Texas extending both west and northeast of Austin. The Guadalupe River flows toward the east and curves southeast for nearly 250 miles in a relatively narrow drainage basin from its headwaters, starting in Hill country and the Edwards Plateau west of Kerrville, spreading onto its floodplain, and finally spilling into San Antonio Bay and the Gulf of Mexico. Average annual precipitation in Hill Country is about 30 inches. Average July precipitation is just over 2 inches, sandwiched between May/June and Sep/Oct peaks. (Average annual precipitation in Texas varies from 10 inches near El Paso in the far west to 60 inches around Houston in the far east, which leaves this targeted region midway between the state’s contrasting dry and wet climates.)

The surrounding Edwards Plateau is underlain by limestone rock formations and thin soils with infiltration capacities that can be quickly overwhelmed by occasional high-intensity rainfall events experienced in these parts of Texas. Sheet flow down the hillsides is rapidly concentrated into narrow channel flows at the bottom of the slopes. According to the USGS, “The Guadalupe River Basin is relatively long and narrow, with a length of approximately 237 miles and a maximum width of about 50 miles. The basin has a drainage area of approximately 6,700 square miles (mi2).” The entire basin has been growing in population to over 600,000. But those headwaters in that steeper northwestern part of the basin are most prone to flash flooding.

Summer thunderstorms in the southwestern states may form when moist air masses move north from Mexico. They are more likely to erupt when afternoon heating destabilizes the air, causing local air parcels to rise and cool to their condensation levels. Isolated storms and narrow cloudbursts such as this are common until unusually wet air masses invade.

Texas flash flood events often begin in the Gulf of Mexico, where ocean water temperatures soar above 80°F during summer months. Such warm water evaporates into warm overlying air masses that have a high capacity to hold water vapor. (Dew points as high as 80°F are sometimes recorded along the Texas coast from summer into fall.) Those air masses are not only full of water, but are charged with tremendous amounts of stored latent heat, waiting to be released when the vapor condenses to form clouds. The muggy air columns often swirl inland into Mexico or directly into Texas, sometimes imbedded in tropical disturbances.

That is exactly what happened during the recent flash floods. After Tropical Storm Barry moved over land and dissipated above the Mexican highlands, its moisture teamed up with additional remnant moisture drawn in from the warm East Pacific (from the other side of southern Mexico). The juiced-up air mass drifted north and became concentrated in pockets caught in a weak unstable low-pressure circulation that stalled over central Texas. Summer surface heating and additional forced lifting up the Edwards Plateau in what is known as Hill Country (which rises up over 3,000 feet) provided the extra instability necessary to build towering severe thunderstorms and local torrential cloudbursts.

Unlike central Texas, the Colorado Plateau doesn’t get direct hits from the Gulf of Mexico. But by the time these Southwest Monsoon air masses arrive from Texas or Mexico, they are capable of generating scattered thunderstorms that can cause damaging and deadly hit-and-miss flash flooding. If you are caught beneath one of these downpours (as seen here coming from this lone cumulonimbus cloud), and not swept away or hit by lightning, you will at least remember it. A few miles away, it’s just another hot summer day.  

The National Weather Service forecast this general pattern days ahead of time and even issued flash flood watches for the region, but these were not the kind of steady and widespread precipitation events common to weather fronts or tropical storms. Many regions of Texas (and some near the worst flooding) received little or no rain, leaving those residents to wonder what was the big deal. Every local Texan has experienced this typical convective summer hit-and-miss instability. Forecasters can warn of scattered thunderstorms and severe weather, but forecast models can’t precisely pinpoint which exact hill or neighborhood will receive the drenching until the local event becomes imminent. Still, NWS tools that include increasingly accurate high-resolution models helped to forecast and follow the massive mesoscale convective system that was developing. Rain rates up to 2-4 inches/hour and local storm totals of 6-8 inches were forecast, though one spot would eventually receive up to a foot or more. Alerts were elevated to flash flood warnings hours ahead as storm locations and severities became more apparent. When individual storms further strengthened and threats increased, wording in the screeching flood warnings became more urgent and desperate, heightened to considerable elevated risk, and finally to a flash flood emergency, which is very rare. (Note the summary of these warnings at the end of this story.) But the communication didn’t make it from the NWS to the victims.  

Gravity took over from there, driving cloudbursts on to the sloping surfaces; sheets of water from above landed to become sheet flow headed to the nearest rill or gully. Within minutes, headwater tributary channels that slice through Hill Country served as efficient conduits as they converged to deliver copious streamflow downhill into the Guadalupe River. Depending on the location, river levels are estimated to have increased from a mere trickle to over 25 feet in less than an hour.

Holiday camps were filled with visitors and some locals who were either out of range of the warnings or had temporarily discarded their phones to celebrate their peaceful weekend in nature. The apparent lack of weather radios and absence of sirens exacerbated the dearth of emergency information, leaving oblivious and vulnerable locals and campers in the dark until the floodwaters were surging around them and it was too late; victims didn’t even have time to make the 5- or 10-minute walk up to higher ground that would have saved them. Hundreds were first stranded and then swept away in another definition of the perfect storm. As the hours passed, peak Guadalupe River floodwaters raced downstream, but passing by populations that were receiving the warnings. Scores of upstream victims, who were incorporated into the cascading flood debris, may never be found in the massive downstream deposits. It seems somehow appropriate that, after being caught in reservoirs and behind dams, the Guadalupe’s floodwaters are headed back to the Gulf of Mexico where all this started, perhaps to evaporate again and continue the hydrologic cycle, or even to fuel the next flash flood event.

Learning from Our Mistakes

There is always a lot of finger-pointing following a disaster such as this. For instance, poorly informed individuals have even been misled with misguided stories about cloud seeding. But cloud seeding efforts have been shown to—at best—increase precipitation from preexisting rain clouds by up to 10%, while no additional precipitation is often the result. And the only company (Rainmaker) that was seeding up to a hundred miles away halted its operations two days before the storms hit. As more information pours in (and it is always easier to second-guess as Monday-morning quarterbacks), what at first seemed to be a tragic and unavoidable series of events may have been averted with some simple precautions: by making sure the camps had access and paid attention to emergency warning systems. A few functional weather radios and/or a siren (such as the one installed just downstream) may have saved hundreds of lives. Relocation of the camps slightly uphill from their previous locations and farther from the riverbed will likely be a future remedy. After all, the greatest number of lives lost were in the epicenter of “flash flood alley”, in the heart of the state that averages the greatest number of flash flood victims each year.

A thunderstorm and its well-defined downburst was caught near Phoenix Airport last year. It’s another example of how one location can be sweltering in drought while heavy rain and flooding is occurring just a few miles away. This photo, taken by Mike Oblinski, appeared in media publications. Now, check out this article and videos showing how these downbursts can become choking haboobs as they drive cool air out ahead of the storm and then push miles across the desert.  

While it has earned our attention, this heartbreaking event represents a motivating opportunity to reevaluate where we develop on floodplains and where we live and set up camp to make sure we aren’t the next victims. And if we travel beyond communication range of the outside world, a good map and some simple research ahead of time could determine whether or not we return safely to share our adventures. It is also an opportunity to recall that for every one-degree Fahrenheit increase in temperature, our atmospheric sponge has the capacity to hold 3-4% more water vapor. In a world of increasing temperatures and hydroclimatic whiplash, what goes up must eventually come down, and this helps to explain why severe rain events and their floods are becoming more common: our atmosphere is loading with greater amounts of water and energy that must be distributed. Meanwhile, we are compelled to ask if such a tragedy could happen in California.               

Are Californians the Next Victims?

It is a bit ironic how both Texas and California exhibit landscapes that suffer from long periods of debilitating drought, punctuated by torrential downpours and catastrophic flash floods. Within hours in both states, concerns about over drafting groundwater resources, lowering water tables, and dried-up springs turn to saving victims from dangerous flooding. Our Golden State harbors a wide range of flash flood environments, especially after fires strip off protective vegetation. All 58 counties have experienced some sort of severe flooding. Look for steep slopes and a lack of vegetation in places that receive sporadic precipitation and you are in flash flood country. Add loose materials weathered on those slopes, and you are in mud and debris flow country. You will find them scattered across the southwest states and you will hear about the latest unsuspecting victims that were swept to their deaths. I have experienced my share of these violent events and I wrote about a few of them in my California Sky Watcher book. I even started my academic career by studying their impacts on landscapes around the White Mountains along the California/Nevada border. But the conditions that lead to our flash flood events are usually quite different from Texas.

Abundant summer monsoon moisture has finally made it all the way into the California desert. Add some afternoon heating to fuel this isolated thunderstorm to develop over the mountains near Barstow. Anyone caught in a desert wash below or downstream from this cloudburst could be swept away.      

During our southwest summer “monsoon”, we only occasionally get incursions of warm, moist air masses from Mexico. Our summer moisture usually sneaks in from the Sonoran Desert or the Gulf of California rather than directly from the Gulf of Mexico, mainly impacting our inland mountains and deserts. Check out our website story from my storm chasing a few years ago. During late summer, rare tropical disturbances (check this video) might even drift up into California (such as Hilary in August, 2023) as they die out. But our “monsoon” airmasses hardly ever arrive as charged up as those Gulf of Mexico surges into Texas. So, our summer thunderstorms are usually more isolated and less severe, producing very little summer rain on the average, even in our desert and mountain areas.

Columns of rain are driven in microbursts out of this summer afternoon thunderstorm and onto the slopes of the San Jacinto Mountains. The alluvial fan radiating out at the center of the photo is littered with boulders the size of cars that have been carried down the fan in debris flows during severe storms such as this one. 

These towering storms are more like afternoon and evening oddities that must build and maintain themselves above smaller specific watersheds in order to power localized flash floods and debris flows. But their rarity is also what makes them dangerous, when they unexpectedly pop up and generate violent flows that can briefly submerge canyons and cough out material on to alluvial fans before spreading into adjacent valleys. Partly cloudy with a chance of scattered afternoon thunderstorms, and a high of 105 or more, can suddenly turn into a violent two-inch cloudburst and deadly flash flood within an hour.

The aprons of alluvial fans that stretch out from the base of our inland mountains, particularly across Southern California and into the Basin and Range, are made of successive mud and debris flows, recalling thousands of years of rare but violent floods that charged out of individual drainage basins long before our developments and infrastructures covered them. On average, these summer events become wetter and more frequent as we travel east into Arizona and New Mexico. Much of the desert southwest east of the Colorado River experiences peak annual rainfall during the summer months. That is why rangers and other officials close some trails in places such as the Zion Canyon Narrows when hit-and-miss storms erupt into the forecast.

This violent summer storm (note the cloud-to-ground lightning bolt on the lower left and columns of rain obscuring landscapes in the background) flooded distant mountain washes, but left this part of the desert dry. 

California’s greatest floods are usually associated with our winter storms’ atmospheric rivers. In contrast to the Texas summer downpours, these larger systems that sweep off the Pacific are forecast long before they come ashore so that we can prepare for them, they bring widespread rain and snow, and they may hang around for days. But the danger and damage can easily exceed many billions of dollars as flooding ravages multiple drainage basins, tests our dams and other flood control infrastructures, and spreads across hundreds of square miles of floodplains after spilling out of surrounding mountains.

California’s most powerful series of atmospheric rivers and resulting megaflood (December 1861 – February 1862) not only lasted for more than a month, but inundated many of our lowlands, including the Central Valley and Los Angeles Basin into Orange County. This event is used as an example for what researchers call the ARkStorm (Atmospheric River 1,000), which is likely to return to do more damage than “The Big One”, the massive earthquake that is overdue along the San Andreas Fault Zone. As examples, floodplains along the Yuba, Russian, and Pajaro Rivers, most rivers pouring out of the Coast Ranges and Sierra Nevada, and most of the Central Valley and Southern California coastal plains are all at risk. Intense downpours that become imbedded in atmospheric rivers and move over burn scars have also powered scores of local mud and debris flows, such as in Montecito in 2018, which killed 23 people. So, we can certainly learn from the Texas tragedies, but we are certainly not Texas (interpret as you wish).

This debris flow devastated parts of Montecito in Santa Barbara County in January, 2018. It damaged or destroyed 500 structures and killed 23 people. Blame downpours delivered by an atmospheric river that followed on the heels of a massive upstream fire. It was one of five such events that have reshaped this landscape during the last 200 years. Photo: Mike Eliason, Santa Barbara County Fire Department.      

What we share with Texas are the increasing amounts of moisture and energy in our atmosphere, warning us how such extreme events are becoming more likely each year. Instead of building developments in harm’s way, we can prepare by leaving spreading basins open at the base of our mountain ranges to catch runoff and allow the pooled water to gradually soak into our aquifers. We can also build more debris basins at strategic locations along water courses to catch debris flows before they invade our settlements and destroy infrastructures. We also share serious concerns about how recent budget cuts and layoffs at NOAA and the National Weather Service will lead to the unnecessary loss of life and property in the future. Let’s all hope that we will be smart enough to prepare for the coming extreme weather events so we won’t have to write future stories about similar tragedies in California.

Viewing toward the Colorado Plateau, it is not unusual to notice towering cumulonimbus clouds and drenching thunderstorms (in the distance) building during summer afternoons just east of the California/Arizona border. It shows that the North American/Southwest Monsoon season is well underway. After sunset, these storms will put on some impressive electrical displays until nighttime cooling finally stabilizes the air. 

Continue below to find some additional sources and a timeline of the Texas flood warnings.

Relevant links:

Guadalupe River Basin Poster

NY Times Texas Flood Sequence

Guadalupe River Rainwater Harvesting

From InFRM: Interagency Flood Risk Management/USGS

Daniel Swain Video at Weather West

Some California Links:
Note how the first two videos look hauntingly similar to the Guadalupe, Texas flash flood. 

The Whitewater River flooded after Tropical Storm Hilary (August, 2023) dropped torrential rains on the San Bernardino Mountains.

Here’s dramatic video showing what resulted when a relatively warm atmospheric river dumped heavy rain on low-elevation Sierra Nevada snowpacks (March 10, 2023), all part of a series of deluges that eventually broke California’s twenty-plus-years megadrought.

A Story about the Megaflood of 1862 and preparing for another.

Burned Watershed Geohazards from the California Department of Conservation.

Central Valley Flood Protection Plan

National Weather Service Budget Cut Impacts

Late July Update: Summer monsoon thunderstorms continued to generate flash flooding across New Mexico into late July, 2025. The mountain village of Ruidoso was repeatedly flooded when heavy cloudbursts poured over upstream burn scars. Here are just two examples of videos floating around out there.     

Here is a summary (from media sources) of some emergency warnings from the National Weather Service leading up to and during the Guadalupe River flash flood event:

Thursday, July 3

The National Weather Service had issued several flood watches for counties in central Texas on Thursday, July 3, warning of the possibility of rain and flash flooding through Friday, but these were not emergency alerts.

11:41 p.m., Bandera County — NWS sends a warning about potentially “life threatening” flash flooding of creeks and streams for residents of central Bandera County, the neighboring county to the south of Kerr County and Camp Mystic. The message includes some standard NWS flash flooding language: “Turn around, don’t drown when encountering flooded roads. Most flood deaths occur in vehicles. Be especially cautious at night when it is harder to recognize the dangers of flooding. In hilly terrain there are hundreds of low water crossings which are potentially dangerous in heavy rain. Do not attempt to cross flooded roads. Find an alternate route.” 

Friday, July 4

1:14 a.m., Bandera and Kerr Counties — This message, the first one for Kerr County, included some of the same standard NWS flash flooding language as the warning sent to Bandera about an hour and a half before.

1:53 a.m., Bandera County — NWS sends a repeat of its earlier first warning to Bandera County (but not Kerr).

3:35 a.m., Bandera and Kerr Counties — NWS sends a repeat of its earlier warning to the two counties, but in the warning language it adds: “It is important to know where you are relative to streams, rivers, or creeks which can become killers in heavy rains. Campers and hikers should avoid streams or creeks.” 

4:03 a.m., Bandera and Kerr Counties — This NWS message, covering the area that includes Camp Mystic, repeats much of the earlier message but is the first to add this more urgent wording: “This is a PARTICULARLY DANGEROUS SITUATION. SEEK HIGHER GROUND NOW!” and “Move to higher ground now! This is an extremely dangerous and life-threatening situation. Do not attempt to travel unless you are fleeing an area subject to flooding or under an evacuation order.”

4:03 a.m. — The National Weather Service in Austin/San Antonio issues a Flash Flood Emergency, stating: “At 403 AM CDT, Doppler radar and automated rain gauges indicated thunderstorms producing heavy rain. Numerous low water crossings as well as the Guadalupe River at Hunt are flooding. Between 4 and 10 inches of rain have fallen. The expected rainfall rate is 2 to 4 inches in 1 hour. Additional rainfall amounts of 2 to 4 inches are possible in the warned area. Flash flooding is already occurring.”

5:34 a.m., Kerr County — NWS sends a repeat of its earlier warning to Kerr County, which includes Camp Mystic. “This is a FLASH FLOOD EMERGENCY for the Guadalupe River from Hunt through Kerrvile and Center Point. This is a PARTICULARLY DANGEROUS SITUATION. SEEK HIGHER GROUND NOW!” and “Move to higher ground now! This is an extremely dangerous and life-threatening situation.”

6:06 a.m., Bandera and Kerr Counties — NWS sends a repeat of its earlier warning to both counties. It reads in part: “Local law enforcement reported numerous low water crossings flooded and major flooding occurring along the Guadalupe River with rescues taking place. Between 5 and 10 inches of rain have fallen. Additional rainfall amounts up to 2 inches are possible in the warned area. Flash flooding is already occurring. This is a FLASH FLOOD EMERGENCY for South-central Kerr County, including Hunt. This is a PARTICULARLY DANGEROUS SITUATION. SEEK HIGHER GROUND NOW!” 

6:27 a.m., Kerr County — NWS sends a repeat of its earlier warning to Kerr County, saying “This is a FLASH FLOOD EMERGENCY” and “SEEK HIGHER GROUND NOW!”

The Guadalupe River reached its peak level of about 36 feet at around 7 a.m. Friday, July 4.

7:24 a.m., Kerr and Kendall Counties — NWS sends a repeat of its earlier warning to Kerr County and neighboring Kendall County, to the east. It reads in part: “A large and deadly flood wave is moving down the Guadalupe River. Flash flooding is already occurring. This is a FLASH FLOOD EMERGENCY for THE GUADALUPE RIVER FROM CENTER POINT TO SISTERDALE. This is a PARTICULARLY DANGEROUS SITUATION. SEEK HIGHER GROUND NOW!”

8:47 a.m., Kerr County — NWS sends a repeat of its earlier warning to Kerr County.

9:04 a.m., Bandera and Kerr Counties — NWS sends a repeat of its earlier warning to these two counties.

Several repeat warnings followed, especially for downstream locations, as peak flooding spread southeast out of Hill Country.  

The following additional images (you may recognize some from previous stories on our webpage or in my book) illustrate summer thunderstorm impacts in California’s deserts.

I often use this visible satellite image to illustrate how moist air occasionally flows up from the southeast into the Desert Southwest and into California during summer. Notice scattered cumulonimbus clouds and thunderstorms popping up during the afternoon from Arizona into southeast California, up along the spine of the Sierra Nevada, and into the Basin and Range. Anvil tops of the storms are sheared toward the northwest within mid-level airflow patterns.
Here’s another image often I use to illustrate how summer thunderstorms can also generate cool downdrafts or outflow winds that sweep across the landscape for miles, kicking up dust, sand, and debris. The violent dust storms are often called haboobs.      
Notice how average annual lightning strikes become more frequent as we move east, away from the stabilizing effects of the cool Pacific Coast summer breezes, and toward land surfaces that quickly heat up.    
It you wait too long, you might be overwhelmed by the power of these violent summer storms as they suddenly build overhead, sweep across the landscape, and deliver driving rainstorms. Stay in a lower wash, and you could be swept away by a wall of incoming flash flood water and debris. Go to higher ground and you could be hit by lightning. You will find this and other summer afternoon storm-chasing scenes on our website story from a few years back.  

Smoke Tree (Psorothamnus spinosus , AKA as Smokethorn), found in our deserts from Mexico and Arizona to southeastern California, may require flash flooding for propagation. Scarification of the hard outer coatings of its seeds occurs due to abrasive action within the tumbling sand, gravel, rocks, and other debris during violent flash floods. This explains why you often find them along desert washes. This beauty is perfectly positioned along a desert wash adjacent to a Palm Springs neighborhood. It shows off attractive purple flowers in late June, but it warns not to build here and to avoid this location during a storm.
Classic alluvial fans such as this one spread out from the base of the Panamint Mountains within the Basin and Range. Tectonic activity has lifted this range and dropped the Panamint Valley along a series of faults. Thousands of years of rare thunderstorms and downpours have carved intricate patterns of rills and gullies on the slopes. The vulnerable, loose materials are mixed with water during such violent storms and coughed out of narrow canyons. The debris has been deposited in fresh lobes, swinging back and forth, one on top of the other, building the fans over time.   
One of my favorite campgrounds at Palm Canyon in Anza-Borrego Desert State Park was destroyed by a debris flow many years ago when a severe summer thunderstorm rumbled directly over the canyon’s watershed. Boulders, giant native palms, and other debris barreled out of the canyon with tons of mud that spread out waste high, encasing picnic tables, bathrooms and other infrastructure.
Badlands topography in Death Valley has been sculpted by rare downpours that impact these steep slopes and carry vulnerable materials downhill during flash flood events. Running water during flash floods is the primary erosional agent even in this landscape that averages only about two inches of rain/yr.
Dry washes such as this one in Saline Valley have been sculpted by rare flash floods that can transport tremendous amounts of sediment.   
After great floods submerged Southern California’s coastal plains, we channeled and paved our rivers in desperate attempts to control nature as millions of new residents flooded in. For many reasons, those mistakes have returned to haunt us. Note the summer afternoon thunderstorms forming over the San Gabriel Mountains in the distance. 
The good news. Summer storms not only bring precious water to the southwest states, but monsoon moisture typically decorates the sky with beautiful clouds and optical phenomena such as this rainbow at sunset. 

THE END

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Wells, Crops, and Crisis https://rediscoveringthegoldenstate.com/wells-crops-and-crisis/?utm_source=rss&utm_medium=rss&utm_campaign=wells-crops-and-crisis Thu, 03 Jul 2025 17:16:23 +0000 https://rediscoveringthegoldenstate.com/?p=5055 Exploring the Spatial Relationships Between Groundwater Depletion, Crops and Landcover in Tulare County, CA. At Rediscovering the Golden State: California Geography, one of our missions is to feature the...

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Exploring the Spatial Relationships Between Groundwater Depletion, Crops and Landcover in Tulare County, CA.


At Rediscovering the Golden State: California Geography, one of our missions is to feature the impactful work of students who apply geographic thought and analysis to pressing California issues. We’re proud to present Jason Runnels, a dedicated student from Santa Monica College.

Jason has completed a significant project titled Wells, Crops, and Crisis: Exploring the Spatial Relationships Between Groundwater Depletion, Crops and Landcover in Tulare County, CA. This timely and insightful work delves into the critical issue of groundwater depletion in Tulare County, examining its spatial relationships with agricultural practices and land cover.

We encourage you to explore Jason’s work by following the link above. Additionally, please take a moment to read his bio (see below) and learn more about his motivations for addressing this critical issue.


A twenty-five-year resident of California, Jason Runnells, the creator behind this featured project, brings a deeply personal perspective to the state’s pressing water resource challenges. With roots in a multi-generational Colorado farming family, he possesses a lifelong appreciation for the intricate relationship between land and water in semi-arid environments. This foundational interest has culminated in a focused exploration of Tulare County’s groundwater issues, a critical component of California’s larger sustainability puzzle.

This project leverages the power of Geographic Information Systems (GIS) to investigate the complex spatial interplay between shifting groundwater levels and established land use patterns. The resulting analysis provides valuable insights for the broader conversation surrounding water management and long-term environmental planning in the region.

Jason’s path to geography and GIS is as unique as his perspective. After a successful two-decade career in the music industry, a desire to more deeply understand the natural world led him back to academia. Under the mentorship of Professor Jing Liu at Santa Monica College, a passion for cartography and spatial analysis was ignited. This newfound dedication to geography has led to an internship as the GIS lead for The Canyon Alliance, where he is instrumental in developing geographic databases and tools to support local disaster preparedness efforts.

Upon graduating this spring with an associate degree in Geography, Jason will continue his studies at UCLA, pursuing a major in Geography/Environmental Studies and a minor in Geospatial Information Systems & Technologies. This project stands as a testament to his dedication and a promising glimpse into a future dedicated to applying the power of geography to real-world environmental challenges.

The post Wells, Crops, and Crisis first appeared on Rediscovering the Golden State.

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Big Ag Vs. Small Regenerative Farming https://rediscoveringthegoldenstate.com/big-ag-vs-small-regenerative-farming/?utm_source=rss&utm_medium=rss&utm_campaign=big-ag-vs-small-regenerative-farming Tue, 17 Jun 2025 03:41:45 +0000 https://rediscoveringthegoldenstate.com/?p=5021 Join us on this field trip into the heart of Central Valley agriculture as we visit two contrasting farms: a small regenerative family farm and then one of the...

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Join us on this field trip into the heart of Central Valley agriculture as we visit two contrasting farms: a small regenerative family farm and then one of the largest agribusinesses in California. We will learn about sustainable farming traditions and the latest cutting-edge scientific research and technologies that power big agriculture.

We all require nutritious meals for our survival. So, the people who grow and harvest our food should be near the top of our list of workers who are rewarded for their labor, right? But that has become wishful thinking as profit margins continue to shrink and more family farms are threatened with bankruptcy each year. Agricultural innovations and revolutions continue to spread, leaving their footprints across California’s landscapes; but current trends too often leave small farmers struggling to pay the bills and keep food on their own tables, all while our popular culture celebrates the latest get-rich-quick millionaires and billionaires who may provide no essential goods or services. California has been the number one agricultural state in the nation for at least seven decades. Our state produces more varieties of farm products than any other state (including some crops that are only grown here commercially), totaling more than 50 billion dollars of income each year.

Upon entering Burroughs Family Farms, visitors are greeted with close-up examples of free-range farm animals.
Burroughs Family Farm is home to happy chickens and other free-range livestock.

Disturbing questions and contradictory data ring out from the Golden State and spread to farming communities throughout the country. How are these paradoxical trends affecting life on the farms and our ability to provide healthy, affordable food to the people? What is the future of agriculture as small farms struggle to retain young people who might continue family traditions? Here, we will dive into these controversies and on to the farms to find some answers. We start with a small regenerative family farm and we end with the largest winery in the world, both just outside Turlock in the San Joaquin Valley, between Modesto and Merced. Our guide is Alison McNally, Associate Professor of Geography & Environmental Resources at Cal State University Stanislaus, and this trip is sponsored by the California Geographical Society.

From left to right, fearless family farmer Rosie Burroughs, our fearless organizer and Stan State Professor Alison McNally, and fearless CSU Northridge Professor Steve Graves gather with curious geographers in front of their store. 

This story is not intended to answer all the questions or solve the many perplexing problems encountered in California’s breadbasket. We have addressed some of them in previous stories on this website and in past publications. For instance, you are probably aware of the controversial debates about how, for decades, big ag has grown at the expense of smaller family farms in California and across much of the nation. Though movements such as farm-to-table encourage sustainable harvests from smaller local farms, many larger agribusinesses have also discovered the economic advantages of more sustainable and/or organic farming on much larger scales. I’ll leave it to you to navigate through the rabbit holes of research and mountains of case studies (such as from UC Davis) that weigh the pros and cons and long-term advantages and disadvantages of small- to large-scale farming. Here, we take you to experience both extremes.

All aboard! Rosie invites us into her hayride trailer for an extended informative trip across Burroughs acreage. 

We’re plowing right into the fields for some first-hand experiential learning, guided by the people who work on the farms every day. We start with a morning tour and informative customized hayride through Burroughs Family Farms and we end with an afternoon at E & J Gallo Ranch. There are some surprising connections to our previous story on this website since, on a clear day, you can see some Yosemite National Park high country when you look east from some of these farmlands. And remember the Merced River than runs through Yosemite Valley? It continues downhill to become a water source for Gallo Ranch, after upstream waters are released from Lake McClure to meander into the San Joaquin Valley. And like the previous story, I am using my personal field notes fortified with a bit of background research. All images are originals taken by me with no tampering or manipulation.

Surrounded by nuts. Rosie points out mature productive trees on the left as they contrast with more recent investments (which are just getting their root systems established) on the right.

Burroughs Family Farms started about 130 years ago in the Berkeley Hills. As Berkeley grew, they paid Burroughs to move toward the Sacramento-San Joaquin Delta, where four dairies were established up to the 1970s.  (We are told that Jersey Island, located where the East Bay meets the Delta, was named after their cows.) When the California Department of Water Resources later bought them out, the family conducted a study, which finally landed Burroughs Family Farms just east of Turlock. They became reestablished as a high producing dairy farm, though their dairies have recently shut down within such a punishing market.

Sheep are grazed on Burroughs property to keep ground cover under control and return nutrients to the soil. No industrial chemicals here.

This is where we meet Rosie Burroughs. We launch into her world of regenerative practices that emphasize how healthy soils grow better-tasting, more nutritious foods. She immediately repeats a valuable lesson from the movie, Common Ground: “If you take care of the soil, the soil will take care of you.” And from Rosie and the next film she recommends, Symphony of the Soil, we learn that “we don’t grow plants, we grow soil and soil grows plants.” She emphasizes how healthy soils encourage infiltration of rainfall to become giant water-holding sponges that are also more pest-resistant. Such sustainable soil water banks increase productivity while requiring less irrigation, cutting the need for synthetic industrial chemicals that may increase yields in the short term, but poison the land and decrease the quality of yields in the long term.    

Barn owl nest boxes as a form of integrated pest management? Studies have shown how owls nesting in the San Joaquin and Sacramento Valley consume pocket gophers, voles, and mice, which are common agricultural pests; it’s another safe and effective form of IPM.

The Burroughs nurtured 20,000 acres for the three years necessary to convert it to organic farming and they’ve been designated organic for 20 years. Now, they grow almonds, beef, chicken, walnuts, and various other products on 12,000 acres. But too many of California’s small farmers have been forced to become price takers rather than price setters. Rosie tells the story of how big ag pushed them out of the dairy business by undercutting their prices and dominating the market. Another unexpected challenge appeared in the form of California’s Sustainable Groundwater Management Act (SGMA), enacted in 2014, designed to ensure the sustainable use of groundwater resources across the state. The one-size-fits-all act restricts use of protective ground cover due to perceived high transpiration rates. Rosie argues that their ground cover is actually cutting evaporation and protecting surfaces from erosion in the long run, as they use grazing sheep and other natural trimming techniques that return nutrients into the soil: “One of the ways they protect and enhance the soil, air and water is by growing cover crops. Continuous ground cover with alternative crops suppresses weeds, improves soil structure, sequesters carbon and attracts beneficial insects and native pollinators. For organic crop production, it also provides nitrogen in lieu of chemical fertilizers.”

The almonds are still green and soft in April, but they will be ripe for harvest, typically late summer into fall in the San Joaquin Valley. It is said that the “l” is lost when they are shaken off the trees, which is why so many mostly older farmers pronounce “am-ond”.
In April, the almonds look like this. They won’t be ready to harvest for about five months. 
Burroughs Farm conserves tons of groundwater with these drip irrigation systems.
Distant views below gloomy stratocumulus skies are all that remain of Burroughs’ dairy after larger competitors flooded the market with competitive products. Imagine the decades of investments and dreams that were lost and abandoned. 
Solar panels and efficient irrigation help to make Burroughs a role model for sustainable regenerative farming.
Free range chickens roam this landscape with mixed uses. 
The farmer on this adjacent property has invested in grapevines. Contrast this landscape with the nut orchards in the background toward the left. Millions of dollars are being gambled when farmers must make such long-term decisions about which crops will be in greatest demand during the years ahead.     
You think they’re proud?
At least 130 years of tradition are celebrated at Burroughs Family Farms.

Though they are busy shipping their fresh farm products around the country, Rosie and family were eager to share their expertise and passion for all-in-the-family sustainable regenerative farming, and we were eager to hear more; but we must move on.   

Alison McNally and other visitors complete their shopping at Burroughs’ little store.
Our leader, Professor Alison McNally, poses with our farmer tour guide, Rosie Burroughs.

It’s time to make the short drive south toward Snelling, where we will learn from farmers who work in what seems to be worlds apart from the Burroughs family … until you look a little closer. This Gallo Ranch was purchased by the Gallo family in the 1970s. Alfalfa and apples have been replaced with rows of grapevines. Their three different acreages in this region (Livingston, Merced, and Turlock) are enormous compared to Burroughs Family Farm, as these landscapes and farming economies define volume-scale winemaking. Founded in 1933 by Ernest and Julio Gallo, their family-owned company became the world’s largest winery, recently raking in revenues of more than $5 billion/year with a total net worth more than $12 billion. 

From left to right, Alison meets up with Gallo’s Brent Sams and Ranch Leader Austin Bartlebaugh, all viewing toward the real stars of this show: the grapevines.

Brent Sams is waiting for us. Brent has been working for Gallo as a viticulture research scientist since 2012. He earned his BA and MA in Geography and his Ph.D. in horticulture and has been researching to understand how fruit chemistry (and quality) changes over time and space. He has used field measurements to test fruit and light exposure, canopy temperature, and soil cores, sensors to measure electric conductivity and elevation mapping, and remote sensing from satellite, unmanned aerial aircraft, and commercial aircraft. It’s a high-tech GPS/GIS environment where updated yields/acre maps illustrate resources put in versus yield coming out. We noted how Gallo employs around 25-30 Ph.D. research scientists on farms scattered around California and beyond. Add paid environmental science internship opportunities. And since Gallo owns only 10-20% of its supply, Sams works with many other farmers who sell to Gallo. In addition to 100 different kinds of wines from around the world, they also sell juice and color concentrates.

During April, sprouting grapevines mark the start of a long, hot growing season on these California ranches. Here, drip irrigation using Merced River water will keep them hydrated.

We also met Gallo’s “smart” autonomous tractor. This $60,000 investment exemplifies (with an exclamation point) how farming is changing fast in California. Turn it on, put it into gear, and the rest is done remotely, sometimes throughout the night. It becomes obvious that, with fewer farmers and more scientists and automation, this is NOT your grandparents’ family farm.

No driver needed. Meet the $60,000 autonomous smart tractor. Just turn it on and put it into gear and let the remote system do the thinking and driving. 

Like Burroughs Family Farms, Gallo uses drip irrigation, but this ranch is also well situated with riparian rights and prior appropriation water from the nearby Merced River. They also plant and occasionally cut nitrogen-fixing ground cover, but they don’t rely on groundwater sources here. Water reigns king as each vine requires between 10-20 gallons/week, and even more during heatwaves. Pumps are only capable of pushing water through about ¼-mile of drip lines at a time. 

Parallel rows of grapevines are spaced perfectly to accommodate this grape harvester, which rolls across the farm, sweeping in the ripe fruit from August into October, depending on the location, grape varieties, and summer temperatures.   

The calendar is also king on these farms. Pruning season peaks during cold and damp January and February and the harvest season runs through August, September, and October, but that has been changing throughout California. Brent provides evidence of the impacts of climate change. Harvest seasons have been getting earlier as grapes ripen faster in higher temperatures. Varieties that require cold nights and big swings in diurnal temperatures have been moving north. Recent extended extreme heat waves are also impacting harvests. So, you might appreciate how the orientation of these rows of grapevines can determine the difference between harvest successes and failures. Rows in California are usually oriented north-south to expose the plants and grapes to just the right balance of sunlight, temperature, and humidity as sun angles change throughout the day. (Hilly terrain, such as in the Napa-Sonoma region, often presents exceptional challenges to these industry norms.) The result is an orderly, repetitious, monoculture landscape that contrasts with the diversity imagined on traditional American family farms.

Sophisticated machinery waits for its time in the vineyards. A host of applications maintains healthy vines to optimized production at Gallo Ranch.

In contrast to some big ag stereotypes, Gallo has demonstrated it is in this for the long run; they’ve invested in a range of sustainable farming methods that regularly win awards and polish their public reputation. And why not be proud of it? Here are some brief excerpts from their website: “As a family-owned company, GALLO has kept sustainable practices as one of our core values since 1933. Our commitment to our founders’ vision has expanded to not only protecting​ our land for future generations, but also improving the quality of life of our employees, and enhancing the communities where we work and live.”

Our group learns that, though this is a big and productive ranch, Gallo owns only about 10-20% of its supply. They work with other farmers around the state and the world to maximize production that totals more than 100 different wines. But it’s time to wrap up this day of action-packed experiential learning.    

And from the Gallo Sustainability Impact Report, “At Gallo, we are leaders in sustainability through our enduring commitment to environmental, social, and economic practices so that future generations may flourish.”… “All of the Winery’s coastal vineyards participate in a unique land management plan started by the co-founders where for every acre of land planted in vineyard, one acre of property is set aside to help protect and enhance wildlife habitat. … E. & J. Gallo Winery has led the way in developing and refining new environmentally friendly practices such as minimizing the use of synthetic chemicals, fertilizers and pesticides, recycling and reusing processed water, creating new wetlands and protecting existing riparian habitats.” Perhaps Gallo has more in common with Burroughs Family Farms than we may have originally thought. 

Whether from a small family farm or big ag, much of our food and drink is produced in the Central Valley. These field experiences into the heart of the valley help us appreciate the work that goes into growing and harvesting what we take for granted, and in decoding the lasting imprints these people and their industries leave on our landscapes, economies, and cultures.

A big thanks goes to Professor Alison McNally for organizing and leading the field trip. Other leaders at Cal State University Stanislaus (such as Professor, Department Chair, and CGS President Peggy Hauselt and professor and former CGS President Jennifer Helzer) worked to make the conference such a success. I am forever indebted to the professionals in the California Geographical Society for championing more than three decades of action-packed scholarly conferences that have informed my teaching and writing, including so many stories on this website. This year, I am particularly grateful for receiving their prestigious Outstanding Educator Award for 2025. After four decades of research, teaching, writing, and putting my heart into such a rewarding profession, this unforgettable conference was icing on my career cake. Thanks to all!    

Here are additional sources for those interested in regenerative agriculture:

Sustainable Harvest International

Foodtank

Farmsteaders Documentary

Alison Mcnally also sent these sources recommended by Rosie:

Common Ground – https://commongroundfilm.org/ streaming on Amazon – a follow up to the film “Kiss the Ground”, Common Ground takes a look at regenerative agriculture and the importance of it as an alternative to conventional agriculture. Some of the footage was taken at Burroughs Family Farms.

TED talk featuring Dr. Jonathan Ludgren (founder and director of Ecdysis Foundation) (13 minutes): https://www.youtube.com/watch?v=okgGmohpaJQ – 

Finally, another Alison recommendation: Jean-Martin Bauer, who has managed food programs and worked as a food security analyst for the United Nations World Food Programme around the globe, is the author of The New Breadline: Hunger and Hope in the Twenty-First Century.

THE END

 

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Cal Naturalists Invade Yosemite https://rediscoveringthegoldenstate.com/cal-naturalists-invade-yosemite/?utm_source=rss&utm_medium=rss&utm_campaign=cal-naturalists-invade-yosemite Tue, 10 Jun 2025 00:49:24 +0000 https://rediscoveringthegoldenstate.com/?p=4923 Follow our UC California Naturalists experiential learning adventures through and around Yosemite National Park for one week as we explore and research natural history within some of the most...

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Follow our UC California Naturalists experiential learning adventures through and around Yosemite National Park for one week as we explore and research natural history within some of the most spectacular landscapes on Earth. I will play the role of student and occasional teacher during our intense daily dawn-evening action-packed learning experiences from April 12-18, 2025, when we earned our official California Naturalist Certificates.

Why Join the Naturalists?

We can’t survive without access to the fresh air, water, food, shelter, spiritual enrichment, aesthetics, personal restoration, and nature’s other essentials that allow us to celebrate life on this third planet from the sun. Our very physical and mental health depend on nature. But our popular cultures have detached us from Earth’s natural systems and cycles, the very forces and processes that rule our world, resulting in perilous dysfunctions that even AI cannot treat or resolve. And have you checked the news lately? Our nature deficit disorders are having tragic consequences that threaten humans, millions of other species, and the very future of our planet.

The UC California Naturalist statewide natural resource education and service program is coming to the rescue! This extraordinary program fosters “a diverse community of naturalists and promotes stewardship of California’s natural resources through education and service.” They draw you in with refreshing truth telling: “We cannot protect and restore California’s unique ecology without an environmentally literate, engaged public.” … and … “Becoming a naturalist offers a chance to explore nature and deepen your understanding of how nature works.” And then they make you offers you can’t refuse: “Are you interested in nature? Do you love CA’s diverse ecosystems? Embark on an immersive adventure with experts. Deepen your understanding of ecology and forge lasting friendships. This course has graduated career starters through retirees, all learning together to become a community of Certified California Naturalists.” How could we resist this magical week in Yosemite?

Follow Us on this Magical Natural History Tour

Join me on this journey as I share some of our day-to-day discoveries from the experts in the field who live this stuff. Images and excerpts from more than 32 pages of field notes prove that, even after leading hundreds of field classes and field trips with thousands of my students and colleagues over more than three decades, we and I will never stop learning. (The stories here are taken from my personal field notes and some occasional background research. All photos are mine and are not edited or manipulated in any way.) Let your curiosity fly like the clouds and wings over Half Dome in this Yosemite natural history expedition.   

Chris Cameron was our organizer, leader, and master instructor for these exceptional learning experiences. Without Chris, a one-of-a-kind tour guide and educator, we wouldn’t be able to retrace our steps because there wouldn’t be any. He demonstrated phenomenal skills in gathering seasoned professionals and curious students together to learn within nature’s living laboratories. And his people skills are the icing on the cake!    

Each day of our expedition gets its own page in this story; simply click to the page that matches the day and/or subject. You are encouraged to follow me chronologically to soak in the full benefits. Here’s how it’s all organized:

Day/Page One (Saturday, 4-12-2025): From the Central Valley up to ECCO in Oakhurst
Day/Page Two (Sunday, 4-13-2025): Geology, Creation, and More than 100 Million Years
Day/Page Three (Monday, 4-14-2025): Healthy Forests and Roaring Falls
Day/page Four (Tuesday, 4-15-2025): Cliffs, Bats, Fires, Technology and Botany
Day/Page Five (Wednesday, 4-16-2025): Following the Trail to Native Americans and American Settlers
Day/Page Six (Thursday 4-17-2025): Grazing, Logging, and Hunting, Oh My!
Day/Page Seven (Friday 4-18-2025): Sharing Our Discoveries

Day One (Saturday, 4-12-2025): From the Central Valley up to ECCO in Oakhurst:

A drive north along Hwy 41 from Fresno eventually takes you out of the Central Valley, which shines as the country’s most productive agricultural landscapes. This sprawling valley is vital in making California the number one agricultural state in the nation, as the state generates well more than $50 billion income per year from farm products.     

Tesoro Viejo is a newly planned community that has sprouted from valley grasslands at the base of the Sierra Nevada Mountains. 

As the road gradually slopes up toward Sierra Nevada foothills, we find ourselves surrounded by open grasslands that recall the vast prairies that once dominated the Golden State’s inland valleys before the Spanish arrived. You will notice cattle grazing on pastoral rolling hills, landscapes occasionally interrupted and sliced by serpentine streams and rivers meandering from east to west, out of higher elevations and into the valley. (These lush narrow riparian strips are what remains (less than 10%) of the broad gallery forests that once extended on both sides of streams and rivers flowing out of the Sierra Nevada.) Today’s hills turn verdant green by April and erupt into rainbow displays of wildflowers such as lupine. But the grasses and flowers will soon dehydrate to the golden browns of punishing summer drought, leaving their seeds in parched soils, waiting for next winter’s rains and next spring’s renewed fantastical displays.

Upon entering the Tesoro Viejo “Hub”, you will be greeted with displays designed to anticipate the future of this growing development and to convince visitors to buy in. 
Here’s how they attract folks looking for activities and new lifestyles with plenty of elbow room.

But another invader has recently rivaled the seasonal nonnative grasses on these gentle slopes at the base of the Sierra Nevada Mountains: humans and their developments. Developers are gobbling up some of these landscapes and attracting people who want to escape urban crowds, chaos, and traffic. “Build it and they will come” continues to spread across these landscapes that tourists have been passing by for decades on their way to the high country. Entire wannabe self-sufficient communities have been sprouting and extending over the grasslands and oak woodlands. And the changes are not coming without controversy. As these ecosystems are scraped up and paved, some locals are watching their reasons for living here disappear, while recent arrivals find relative peace and quiet in their perceived bucolic settings. Talk of limited water and other resources, habitat destruction, loss of open spaces, pollution, land values, affordable housing, and increasing traffic congestion is replacing the traditional agrarian discourse and cultures. Such noticeable changes are stretching and then redefining our perceptions of wildland-urban interfaces. The end of this world as we knew it may be just one more development away.

Who do you think these displays at Tesoro Viejo are designed to entice? The image here is all about image. And it’s just more than an hour to the Yosemite National Park south entrance. The English translation is “old treasure”, but the developers prefer to use “ancient” treasure. 
Real or imaginary? Sprawling grasslands and rolling foothills await; now, all you need are the toys, after you are convinced to invest. Inside the “Hub”, the restaurant and community meeting areas are just behind us.
Tesoro Viejo is one of numerous planned communities that have been developing their way along the base of the Sierra Nevada. But locals and newcomers are noticing increasing traffic congestion and other problems that accompany such growth.    
Making our way up to the foothills and tablelands along Hwy 41, we see plenty of open land for sale, just waiting for the next developer with deep pockets. 
Bucolic rolling hills emerge above the valley as we continue north along Hwy 41. Afternoon fair weather cumulus clouds boil up over the distant high country.
As we approach 2,000 feet above sea level, where it is slightly cooler and wetter, we notice oak woodland plant communities. 
At just above 2,000 feet, dry pines and other species join the oaks to cover the hills. In the distance, notice how the hotter and drier southwest-facing slopes (facing toward the afternoon sun) support fewer trees, while the cooler, moister northeast-facing slopes (facing away from afternoon sun) are lusher. In the foreground, the house is surrounded by a mix of native and nonnative species. The fire hydrant reminds us that we are in a classic wildland-urban interface that is more wild than urban, where annual wildfires threaten for at least a few months each year.
Native American and Gold Rush history are celebrated in numerous towns scattered around Sierra Nevada foothills. This is in Coarsegold along Hwy 41 on the way to Oakhurst.  

Once we get up above about 1,000’ elevation, where a little more precipitation falls and temperatures are a bit cooler, an assortment of scattered oak trees pops up above the ground cover. At about 2,000’, the woodlands thicken and diversify to include gray pine and other drought-tolerant trees. These scraggly pines with long, grayish needles and big cones often appear bent and twisted as though they were dancing through the night and were suddenly frozen in a pose by the morning light, waiting for summer’s fire or winter’s first merciful rehydrating showers. As we progress higher, slopes tend to steepen and we notice mixed pine forests as we look up toward snow in the distant high country. (We will revisit Sierra Nevada’s vegetation zones in more detail during the next few days.) We drop down into the town of Oakhurst (elevation 2,274’), nestled in its little valley that many consider the gateway to Yosemite. Traveling up and a little farther north, we finally turn off Hwy 41 and will settle, hang our hats, and share tasty meals at ECCO each night, which is a pretty typical option for tour and educational groups looking for base camps in and near Yosemite: “The Episcopal Conference Center Oakhurst (ECCO) has been serving the religious, educational and non-profit conference and retreat needs of Fresno, Madera, Mariposa and the rest of California’s Central Valley since 1982.”       

We are at about 3,000 feet above sea level, looking down at Oakhurst, which is nestled in its little Oakhurst Valley along the Fresno River. Notice how the woodlands have become denser as we approach higher elevations. In the distance, afternoon cumulus clouds pop up above the snow-covered Sierra Nevada high country. 
At ECCO, arriving students congregate around a road kill (which happens to be a male California quail) that we will use to attract whatever wildlife might roam onto the property.
This field camera (on the right) should capture images of any curious or hungry critters that wander into view. 

This is where we can hear Yosemite calling from just several miles away. The rolling landscapes in and around ECCO (about 3,100’ ASL) is populated with mostly open oak and pine woodland. The deciduous oak trees are just beginning to sprout by mid-April, careful to avoid any late-season freezes. A giant pond with a fountain demands attention, decorating the property and attracting more than our senses. Depending on the season, an assortment of waterfowl and other wildlife visit or live around the water (more than 100 species of birds have been recorded there), demonstrating animal behaviors that deserve a line or two in our field notebooks.

Chris Cameron (“naturalist guiding in Yosemite, teaching UC California Naturalist programs, and sparking immersive nature experiences”) introduces participants to the program, kicking off our week of extreme experiential learning in and around Yosemite. 

Wild turkeys are particularly entertaining as they dive out of their trees (where they roost at night to avoid predators) early in the morning and trot around during the day. Their toe-walking and dragging one foot in front of the other leaves an arrowhead-like trail. Turkeys are not native to California, but numerous attempts to introduce them finally became successful so that their numbers multiplied since the 1960s until they now total about 250,000 in the state. These omnivores mate and lay their eggs during spring. Gestation takes about a month and they are most vulnerable to predators (such as coyote, bobcats, foxes, some birds, and domesticated animals) after hatching. Adults may become nuisances around humans as they show aggression with their flapping and pecking; their droppings also get pretty messy. They’ve been known to damage gardens and attack their reflections in windows and on the sides of cars.  

Wild turkeys trot around the ECCO property.

The turkeys remind us that every species of plant and animal, every landscape, rock, cloud, water drop, and weather event have captivating natural history stories to tell. Informative and useful narratives grow from research that connects all of us to our natural world. We can see why this is just one of the naturalist programs across the US. Master instructor Chris Cameron started our course by summarizing how we celebrate biodiversity with environmental literacy, scientific and social understanding, by honing our interpretive skills, and practicing collaborative conservation. We reviewed our state’s bioregions and geomorphic provinces (from page 29 in our required California Naturalist Handbook), which coincide with the physiographic regions we have explored in numerous stories on this website and in my publications. And we recognized how the California Floristic Province, a biological hotspot with its thousands of species that include a large percentage of endemics, is experiencing a biodiversity crises as increasing numbers of those unique plants and animals are threatened with extinction. We recognize how naturalists’ work has become crucial as we observe, communicate, and act to build essential links between scientists and the average person. After dinner, our first day and evening ended with my presentation that summarized some fascinating properties of water and the weather patterns and climates that rule over our plant communities, topics we have highlighted on this website and in my recent California Sky Watcher book and statewide tour.      

The pond at ECCO is the center of attention, attracting diverse wildlife species from around the region and visitors from beyond.

Click (below) to the next page and day.

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Cataclysmic Aftermath Landscapes https://rediscoveringthegoldenstate.com/cataclysmic-aftermath-landscapes/?utm_source=rss&utm_medium=rss&utm_campaign=cataclysmic-aftermath-landscapes Wed, 12 Feb 2025 06:49:43 +0000 https://rediscoveringthegoldenstate.com/?p=4872 Most of you have already seen the inconceivable destruction on local news and social media. After surveying post-fire landscapes from Malibu to Pacific Palisades, and from Eaton Canyon to...

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Most of you have already seen the inconceivable destruction on local news and social media. After surveying post-fire landscapes from Malibu to Pacific Palisades, and from Eaton Canyon to Altadena, I am sharing images that help summarize the extent of devastation just about a month after the conflagrations. The two previous stories on this website summarize conditions that led up to these historic disasters.

There are at least five main themes threading through these images and videos. First, the steep slopes, loose materials, and stripped ground cover leave landscapes vulnerable to any significant precipitation, especially heavy downpours. Such mud and debris flow threats will continue with every rain event until sometime in April, when our normal annual wet season usually ends. Then, there’s always next year. Second, note the haphazard and unpredictable burn patterns that determined which homes, neighborhoods, and businesses were destroyed and which survived the firestorms as they swept through. Third, many of you may have to strain to recognize what is left of some iconic SoCal landscapes and neighborhoods seen and celebrated in countless films, TV series, commercials, and videos over the decades. Fourth, note how the wildfires didn’t discriminate, ravaging diverse neighborhoods from rich to middle- and working-class. Finally, we will end with a few articles that summarizes how we built ourselves into this disaster-prone corner.

Burnt landscapes rise up toward a wisp of fog and high cirrus clouds. One month before January’s calamities, the Franklin Fire raced through Malibu Canyon. As relentless Santa Ana winds blew it toward the coast, it surrounded but spared Pepperdine University (on the left) before reaching PCH.

I am also sharing the following images to confirm that there is no reason to visit the devastation, since you are not likely to discover anything new that hasn’t already been displayed multiple times in the media. And there are at least five reasons (yes, another list!) to NOT go wandering into the Palisades or any other recently burned areas. First, PCH and other roads along that entire coastline and into the Santa Monica Mountains will be subject to closures at least through what remains of our rainy season. Second, even if you find an open road, the one-lane traffic gridlock is a frustrating waste of time. Third, you can’t turn off or even briefly stop without getting cited (at best) or arrested by an army of law enforcement officers. Fourth, these are toxic landscapes that pose a host of health hazards and dangers to visitors. Finally, cleanup and construction crews are working hard to rebuild essential infrastructures throughout Pacific Palisades and Altadena. The last obstacles they need are selfie crowds getting in their way and impeding their progress. So, as you view immediate post-fire images here and in the media, know that there is nothing more to see as the cleanup progresses.

Though the December, 2024 Franklin Fire was fanned out of control by high winds, it burned through landscapes in Malibu Canyon that had been torched just a few years earlier. Could the lack of mature fuels be one reason why it didn’t burn hot enough to incinerate everything down to the ground? Still, foreground and background slopes on each side of Malibu Canyon were singed by the Franklin Fire, leaving them vulnerable to erosion and mass wasting.

The Mountain and Franklin Fires as Warnings

Two months before the mass destruction in LA County, the Mountain Fire erupted in nearby Ventura County. Strong Santa Ana winds (as predicted) also fanned this blaze that consumed nearly 20,000 acres and 243 homes and commercial structures. Just about one month later, the Franklin Fire ignited on Dec 9 and quickly grew to 4,000 acres as powerful Santa Ana winds (again, as predicted) funneled through the Malibu Canyon wind tunnel and toward the beach. In contrast to the Palisades and Eaton fires, it only destroyed or damaged 48 structures, including a few homes. For instance, Pepperdine students and staff were forced to shelter in place as the flames raced around them, but the campus survived. Heroic efforts by savvy firefighters helped to contain the damage, but it also helped that Malibu Canyon had burned just several years earlier. Researchers use the historical record to estimate that this area has burned in wildfires on an average of two times/decade (the entire Malibu coastline is impacted by even more frequent fires), which decreases potential fuel build ups. But such frequent fires also encourage the invasion of nonnative species that are more flammable, leading to even more frequent fires and accelerated wildfire growth. By most Decembers, our fire season has been snuffed out by winter rains. (Rains brought welcome relief months earlier in the previous two years.)  But this year’s long drought dragged, incredibly, into late January, through the middle of our rainy season. The stage was set for relentless Santa Ana winds that would take over from there. As finger pointing mounts about details and specific responses to these wildfires, here are a few facts to keep the debates honest.

Nearly four years ago, I posted a story about The History of a Grain of Sand. You will find it a few pages back on this website. There, you will also find a photo showing this landscape (years between fires) covered with green coastal sage, chaparral, and riparian woodlands. Here’s the copied caption: “Dams as Barriers to Sediment. The Rindge family built the Malibu Rindge Dam in the 1920’s. Its reservoir filled with sediment carried by Malibu Creek within a few decades and it was never fully functional. Malibu Creek might not look like much during the dry season, but it can become a raging torrent with very high sediment loads during winter storms. The sediment trapped behind the dam was destined for Malibu Lagoon and today’s world-famous Malibu Surfrider Beach. Many other beaches along California’s coast have been starved of sand and become more erosional due to such upstream obstructions. This is among several of the state’s obsolete and useless dams that have been targeted for demolition to restore their streams’ ecosystems and allow migrating fish to return and spawn. Enormous costs have slowed such restoration projects.” Now, after the Franklin Fire, we can see how sediment yields from these steep slopes with loose materials will rapidly choke Malibu Creek as they flow down to Malibu Lagoon during rainstorms. Notice how the wildfire blew away from upstream slopes (in the distant left) that are still covered with thick chaparral.
Notice how the burned slopes on the right will be vulnerable to erosion, while the unburned riparian canyon bottom and chaparral slopes in upstream Malibu Canyon (on the left) will gradually absorb and release water, slowing denudational processes.
This satellite image (taken on December 13, 2024) shows the extent of the Franklin (Malibu) burn. Notice the darkened surfaces surrounded by red fire retardant at the very center of the image. Downstream Malibu Lagoon and Surfrider Beach point toward the ocean and away from Malibu Canyon and the fire scar. Pt. Dume is on the far left and Pacific Palisades (not yet burned) stretches beyond the far right. Source: NASA Earth Observatory Landsat Imagery.

Unraveling Some Misconceptions

First, these firestorms had nothing to do with water diversions from Northern Cal. The state had just experienced two consecutive banner wet years that finally broke our two-decades-long megadrought and then competed for the wettest on record. Nearly all of our reservoirs were recently filled and our state water projects overflowed with more water than we could distribute and use. Unfortunately, the several months of recent unprecedented drought that followed those storms dehydrated the biomass that accumulated during the previous two rainy years, providing abundant dry fuels for ignitions. Our state’s water diversion and storage projects were performing well, but were surrounded by dehydrating Mediterranean plant communities interspersed with encroaching human developments, all enduring prolonged and historic Santa Ana winds. Only the details were left to debate in this landscape made for disaster, where millions of Californians found themselves within an expanding wildland-urban interface.

Before the firestorm, multi-million-dollar homes lined Malibu Beach near Topanga. These lifestyles seemed worlds away from working- and middle-class Altadena, but their people and communities would be tragically linked when Santa Ana winds drove separate wildfires of destruction in early January, 2025.

As example, the one relatively small reservoir that served Pacific Palisades had been “taken out of service to “meet safe drinking water regulations,” the DWP said in a statement. A tear in the reservoir’s cover made the water supply subject to contamination, the Los Angeles Times reported, leading the agency to drain it in February.”  … (meaning last Feb.). This left three one-million-gallon tanks to serve the Palisades, which were more than adequate for providing safe drinking and irrigation water and for fighting multiple structure fires. They obviously weren’t enough for fighting the stampeding wave of flames. Many fire hydrants designed to battle structural fires and smaller brush fires were also inadequate for such a colossal bombardment. Such details will be the focus of investigations into how heroic firefighters could have had a better infrastructure to support their efforts as winds peaked over 70mph. Many scientists, engineers, and firefighters question whether ANY water infrastructure could have made much of a difference in this firestorm fanned by wicked winds that also hampered air assaults. This was also the case in the Altadena inferno, where fist-sized burning embers were being blown up to a mile ahead of the fire front. 

We thought that rising sea levels and giant waves would eventually take these upscale houses that were sandwiched between PCH and the surf, as they did in some previous storms (such as in the historic 1982-83 El Niño year). But when seasonal rains went AWOL, nature attacked from the opposite direction in January, 2025. Santa Ana winds drove the flames all the way to the beach, destroying investments, dreams, and stereotyped SoCal lifestyles.

Finally, for those of you not familiar with SoCal, our wildfires that spread into neighborhoods did not (and usually don’t) erupt and spread from a “forest’, but from our coastal sage scrub, chaparral, and related plant communities that help define our Mediterranean climates and ecosystems; so, “forest” management is not relevant. We’ve heard suggestions that our plant communities should be destroyed to protect nearby developments, but that would require clearing at least half-mile strips surrounding every structure. This would represent habitat destruction on a massive scale, accelerate species extinctions in our unique California Floristic Province, and wipe out thousands of natives and endemics. And they would likely be replaced by invasive nonnative grasses and other highly flammable biomass that act as conduits for fires. Proposed “clearance” on such a grand scale would also result in more frequent and catastrophic floods and debris flows out of these disturbed, vulnerable landscapes during nearly every rain event. We’ve seen this movie and its sequels play out too often: the very plant communities that protect us by absorbing floodwaters and stabilizing our slopes, provide habitats for a dizzying array of plant and animal species, and represent open spaces where we can appreciate and study our natural history, can suddenly turn on us by sending their burning embers.

Opulent lifestyles were on exhibit when this home along Malibu Beach near Topanga was selling just a year before the wildfire torched this coastline. Watching the waves crash just below the deck, I asked the real estate agent if he thought buyers would have any trouble finding insurance; he replied as if he didn’t know. Neither of us were thinking about wildfire threats. I now wonder who bought it and how they are coping.

Our careless developments and dysfunctional relationships within these very ecosystems that we cherish have been debated for decades and these difficult debates will (and should) continue into the future. It took many decades to build ourselves into this worst-case scenario fire corner. For more objective analyses and some back-to-reality answers, check out the links that follow my aftermath images, at the end of this story. As you view the following images, please remember that they are what remains of thousands of families’ hard work over many decades … shattered lives, hopes, and dreams incinerated into ashes.

After ravaging the Palisades, the firestorm jumped down this slope and crossed PCH, finally stopping at the Pacific Ocean.  
The Reel Inn was a landmark along PCH where families and friends were reeled in by their catchy puns-of-the-day and tasty fish dinners. This is only one of hundreds of businesses that were destroyed in the Palisades Fire as it raced to the ocean. The chilly fog that was once dreaded by beachgoers was suddenly seen as a friend, drifting in contrast to the high winds and single-digit relative humidity that fanned such destruction.
The blue sign reads Malibu. But don’t go through the cones! Here’s the border where we drive from Pacific Palisades into Malibu. PCH was briefly open to one lane each way before mudslides closed it again. Rows of beach homes that once extended along the shore in the distance have been burned to their foundations. Fire weather is just a memory in the cool, misty fog that hugs the coastline on this day.
Residents in these beachside properties were shocked to watch giant burning embers flying off the coastal slopes and across PCH, igniting one home after the other. The “Santa Ana winds blowing hot from the north” were once celebrated for delivering warm, sunny fall and winter beach days to SoCal as the rest of the country was freezing. Not this time. By contrast, this shroud of fog was a welcome sight.
Residents of this beachside home didn’t have time to save their car or other possessions. Some were lucky to escape.
This car was parked in front of a home that burned into the sea. Their stairway to heaven is all that remains of another beachside retreat.
These chimneys might have been used on foggy days such as this one, when temperatures can drop into the 50s, and beachside residents might complain about how “cold” it gets in the winter.
Can you see those green tubes? California’s Office of Emergency Services warns us not to move them: “Cal OES has tasked the California Conservation Corps (CCC) [workers in white jumpsuits and hardhats marked “CCC”] to place compost silt socks [long green tube-like material] and other protection material like straw wattles [long burlap tubes] and silt fences around residential and public areas including sidewalks or roads. You may also find these materials around storm drains.” The barriers are particularly important here, since the surf is already contaminated with toxins falling and washing in from the burned structures and fire zones, forcing health warnings all the way down to Santa Monica and Venice.
No longer living on the edge. We built as far west as we could go, until the ocean represented the last barrier to development. Imagine climbing these stairs to your third story as you look out across the Pacific Ocean during one of those cherished sunny, warm beach days. Who would believe that the final threat would come as a flaming bombardment from the sky?
These stacked K-rails will soon be lined up along the base of the slopes to keep mud and debris from flowing on to roads and other infrastructure. They work for moderate storms, but they are no match for prolonged heavy rains that can generate powerful mass wasting events.
These were not your grandmother’s mobile homes. This mobile home park along PCH was the last most “affordable” choice along such an exorbitantly expensive coastline. I often wondered what it was like to live there and now I wonder if anyone will ever return, since the Palisades Fire burned it all to the ground.   

Before we skip inland over to Altadena and the Eaton Fire aftermath, here’s just one example of what was lost in the Palisades. Some folks who couldn’t afford to buy a house on the beach opted for a mobile home and also lost everything. This real estate description paints a pretty clear picture of life there in the before times:
16321 PCH
Pacific Palisades Bowl Mobile Home Estates
Roughly $500,000-$1 million
What’s special
BREATHTAKING DRAMATIC OCEAN VIEWS MARBLE BACKSPLASHES CUSTOM CABINETRY EXPANSIVE MASTER SUITE SEPARATE PANTRY ROOM QUARTZ COUNTERTOPS HIGH-END FINISHES
MOVE-IN READY! This stunning, new construction custom-designed, 2-story beach home is perfectly positioned across from the iconic Will Rogers Beach in Pacific Palisades, offering an unmatched combination of luxury, convenience, and coastal beauty. The home’s prime location provides breathtaking, dramatic ocean views from Malibu to Catalina Island, visible upon upper level. Entering, you’ll be enveloped by a bright, open ambiance that seamlessly merges indoor and outdoor living. Natural light floods the home, illuminating the carefully crafted details throughout. With 2 bedrooms and 2 bathrooms, this home boasts soaring 9-foot ceilings and elegant double-door entries that enhance its spacious, airy feel. The first floor offers a convenient bathroom, while upstairs, the expansive master suite awaits with a dual-entry bath alongside a second well-appointed bedroom. Every inch of this home has been thoughtfully curated with high-end finishes, including quartz countertops, marble backsplashes, and custom cabinetry with pull-out shelves in the chef’s kitchen. The kitchen is equipped with premium stainless steel appliances, a Shaw’s farm sink, a gas oven, vented exhaust fan, disposal, refrigerator, dishwasher, separate pantry room, and stackable washer and dryer. Additional features include central heating and a tankless water heater, enhancing both comfort and efficiency. Outside, imagine crafting your ideal outdoor retreat on a spacious 320-square-foot second-story deck, perfect for lounging and entertaining while soaking in the endless ocean views. Dedicated two parking spaces and guest parking available, and 24-hour private security patrol. Residents enjoy access to premium community amenities, including a large heated pool, hot tub, billiards room, and a recreational area. Positioned near Palisades Village and top-rated schools, this home combines luxury with practicality. Cross PCH via a nearby crosswalk for quick beach access, and enjoy low space rent of $970/month with rent control, plus the added financial benefits of no annual property taxes or HOA fees. Purchase includes city and coastal approved plans for custom built deck for convenience.

Eaton Fire (Altadena) Aftermath

Altadena is only about 25 miles (straight line distance) northeast of the Palisades, but most locals would tell you that they seem worlds apart. It can take about an hour (depending on traffic) to navigate from one to the other and you might feel that you’ve been transported hundreds of miles from a beach once you finally arrive in Altadena. Adjacent to Pasadena of Rose Bowl and Parade fame, Altadena is nestled on the edge of the San Gabriel Valley at the base of the San Gabriel Mountains. It looks up to the abrupt steep slopes (once covered by chaparral and woodlands) that tower all the way up to Mt. Wilson, all being lifted along a series of active faults. Cooling sea breezes often struggle to make it this far inland during hot summer days when the smog can get caught below the infamous inversion and jammed against the mountains. By contrast, during winter, this region can resemble a warm, sunny paradise when their spectacular snow-clad mountains point into crystal clear blue skies.

Compared to the Palisades, Altadena displays cultural diversity that is more representative of California. This is partly because the neighborhood known as Altadena Meadows was one of the few communities where black families were allowed to settle, back during the days when segregation was enforced and redlining ruled. Thousands of working- and middle- class families worked hard for decades to improve these neighborhoods, often hoping to pass their investments on to future generations. I learned about Altadena when I frequented Pasadena, enjoyed hikes into the local canyons, and developed a working relationship with the heroes of the Eaton Canyon Docents, led by Diane Lang. There at the renowned Eaton Canyon Natural Area and Nature Center, we trained docents to guide school groups and visitors eager to learn about the natural history of these treasured Mediterranean landscapes. We learned a lot of science while exploring the natural systems and cycles that rule our world and we soothed plenty of nature deficit disorders.

All of it has been lost. Surrounding slopes, the nature center, homes of some of the docents (including Diane’s house), much of Altadena and more of Altadena Meadows has burned to the ground. We always studied and understood how fire plays such an important role in these ecosystems and locals even recalled when another wildfire burst out of the mountains and burned the old nature center in October, 1993. But this fire was different, as it was fanned by the fiercest Santa Ana winds that blew burning embers a mile ahead of the front. Just as the Palisades Fire was destroying everything in its path all the way to the beach 25 miles away, this fire would not stop at the base of the mountains. It was blown ahead right into the city, destroying entire neighborhoods that most people thought were far removed from wildland fires. Within one tragic day and night, Altadena and Pacific Palisades were connected in ways that some could not have imagined. The two previous stories on this website summarized the conditions that led to these tragedies and why they exploded out of control. But perhaps the key word is control. Nature’s awesome power reminds us that we cannot separate ourselves; we are just parts and players within these natural systems and cycles.

Homes above and around Eaton Canyon were haphazardly torched as winds blew wildfire embers across the sky. Entire downwind neighborhoods would be next to experience such terror.
Homes just above Eaton Canyon were lost while the fire stripped surrounding slopes (in the background) down to ground level. It won’t take much rain and runoff to move that material downslope.
It will take a long time and a lot of work just to clear homes and neighborhoods of the toxic debris that was exposed by the fires, but lessons learned from previous calamities are being implemented.
Hundreds of businesses and houses of worship were also victims.
Landscaping and homes were destroyed, leaving the burnt shells of chimneys, trees, and vehicles. Notice how the car is painted with NOT EV, meaning there are no toxic EV batteries there. Also note the barren slopes stripped of vegetation in the background.
An army of cleanup and construction companies are advertising in the fire zones. Even before the conflagration was fully contained, some families were already getting notices from predatory real estate investors and developers asking to buy their properties. Residents will be challenged to restore the character of their burned-out neighborhoods.
This corner home at Altadena and Page was one of thousands destroyed within these neighborhoods. Decades of history and unique architecture were lost in the wildfires.
Those long green barriers (AKA silt socks) are not to be moved, since they are containing toxic runoff that could become problematic during rainstorms.
It’s a disaster landscape with thousands of lone chimneys and collapsed tile roofs.
Paradise was interrupted, replaced with thousands of windows and entryways into burning nightmares.
The Eaton Fire barged right into town, burning businesses and just about everything else in its path. Look carefully to see the skyscrapers in downtown LA sticking up in the background.
Another Altadena entryway to the lost before times.
Classic cars were among the victims here. Imagine all the years of work, love, and care that went up in smoke.
NO EVs on this lot, but this entire section of the Altadena Meadows neighborhood is gone.
Step one is complete here, but recovery efforts will take years and countless more steps.
Looking for before and after scenes? Here’s one example of a local artist who is making a positive difference in Altadena Meadows: https://www.youtube.com/watch?v=nYPmFS84SiA
It looks like someone has gathered what remains of potential toxic substances from this burned-out home.
The Eaton Fire burned into Altadena right up to their fire station.
Only the singed fence and a few trees “survived” total destruction on this corner lot in Altadena right across from their fire station.
Preparing for the sediment attack. When the rains come, it is hoped that these catch basins at the base of Eaton Canyon will be sufficient to keep mud and debris flows out of what is left of adjacent Altadena neighborhoods. There’s not much time here as a storm and atmospheric river was forming over the Pacific.
Ready for the next “natural” disaster? Only a month after the fires, residents and officials received sufficient warning from forecasters days ahead: the next drama would come from an atmospheric river that could dislodge loose materials off of the unstable burn scars.

In case you missed it, positive messages and messengers of hope are gradually rising out of the ashes in Altadena. Here’s one example of a local artist who is making a difference in Altadena Meadows. It includes some video from the air: https://www.youtube.com/watch?v=nYPmFS84SiA

This interview confirms how a reality check and building paradigm shift is necessary if we expect to develop more fire-resistant communities. (Thanks to Bill Patzert for sending it along.)

This is a very thorough summary of the corner we have built ourselves into, and our long LA fire history. Thanks again to Bill Patzert for sharing.

Here’s another LA Times article that sums up the problem and some potential solutions.

This Malibu Times article is dated, but leaves us with a rough fire history up to 2007.

If you’re in to geospatial imagery, check out these before and after NASA EARTHDATA images captured in January, 2025, by the MSI instrument aboard ESA’s Sentinel-2A platform.

This camera shows the advancing smoke and flames that eventually consume a Pacific Palisades neighborhood.

This video (it is a long journey) takes you up from PCH through Topanga Canyon in the aftermath to see what burned and what escaped the flames, illustrating why any substantial rain will produce destructive mud and debris flows. It was filmed on January 17th.

Here is a Pacific Palisades Aftermath Tour.

Let’s hope this will be THE END of our disaster stories for a while.

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Making Sense of our Apocalyptic Firestorms https://rediscoveringthegoldenstate.com/making-sense-of-our-apocalyptic-firestorms/?utm_source=rss&utm_medium=rss&utm_campaign=making-sense-of-our-apocalyptic-firestorms https://rediscoveringthegoldenstate.com/making-sense-of-our-apocalyptic-firestorms/#comments Sat, 11 Jan 2025 10:34:03 +0000 https://rediscoveringthegoldenstate.com/?p=4779 This week represents the line between the “before times” and “after times” In Los Angeles County and perhaps California. It is not hyperbole; it’s the new reality. Southern California...

The post Making Sense of our Apocalyptic Firestorms first appeared on Rediscovering the Golden State.

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This week represents the line between the “before times” and “after times” In Los Angeles County and perhaps California. It is not hyperbole; it’s the new reality. Southern California will never be the same. And everyone finally understands that, no matter where or who you are, no person or community is immune to the ravages of nature’s awesome power when we create such imbalance. I’ve been posting stories and writing books about these realities for years. You will find them on this website and peppered throughout my California Sky Watcher book. As of this writing, we count more than 57,000 acres burned, at least 29 deaths (with more human remains still being discovered), more than 16,000 homes, businesses, and schools destroyed, and at least $250 billion in damages and recovery costs. After nearly 200,000 people were evacuated and far more lost power, entire neighborhoods and business districts were wiped out, and some of California’s most cherished natural and human landscapes have burned beyond recognition in just a few days. You can go to your TV and social media to get the dramatic, heartbreaking, and often gory details; this time, the sensationalists don’t have to exaggerate.

Here is a deeper story that explains how this happened, but more importantly, why it’s happening now. I will guide you through the play-by-play, always emphasizing the science behind the scenes, so you can see that this catastrophe is not past tense, no matter how much later you are reading about it. To set the stage, make sure you wander through our previous website story about precipitation extremes to understand how we got here.

This spectacular roll cloud was photographed from New York Drive at Eaton Canyon Wash in Pasadena looking west on January 7, 2025, 7:30am. It is an example of a rotor cloud that formed on the lee side (downwind) of the mountains. High velocity stable air was forced up the opposite sides of the mountains until it reached the top. There, the relatively heavy air was liberated to tumble down this leeward side (from right to left, since it’s an offshore Santa Ana wind) past its equilibrium so that it had to rise up again as it races toward the coast, meandering up and down roller coaster style within repeating mountain waves. But a vertical circulation has formed on this leeward side. Stationary clouds condense on the top section of the rotor where air cools as it rises. Such clouds signal turbulent air and this one is an ominous precursor to the windstorm that will fan a deadly and catastrophic wildfire across Altadena and Pasadena later in the day. Photo by Matt Wright. UPDATE: Here is Matt’s message he sent with this photo: “It’s pretty violent up here right now. Top gust so far is 50 mph, but steady winds are around 30, with gusts in the low 40s. We’re all fine, but packed and ready to bug out in case of fire in the hills above us.” Sadly, their house was one of the first to burn in the deadly Eaton Fire. 

Two years of heavy rains + a record nine months of drought + epic windstorms + low humidity all along the wildland-urban interface = …

It started with two years of record rainfall (competing for the most rain ever recorded in the Los Angeles area during two consecutive years), which finally broke our more than two-decades-old megadrought. Rehydrated plant communities flourished. Ecosystems added tons of biomass. Grasslands, coastal sage scrub, chaparral, oak woodlands, riparian woodlands, and every other plant community joined the party. As usual, the rain stopped last spring to make way for summer’s drought, starving our Mediterranean ecosystems of water. Through the autumn months, as water content in our plants dwindled each day, the annual race was on to see which would come first: Santa Ana winds or the first rains. Substantial early rains typically douse the fire season until next year. But, as I mentioned in the previous story on this website, the storms didn’t even show up for this year’s competition. SoCal’s widespread rainfall totals since spring remained near or below ¼ inch by mid-January, the middle of our rainy season. (As example, LA Airport had recorded only 0.04 inches and Santa Monica was at 0.09 inches for the water year well into mid-January, making this compete for the driest stretch on record for the region.)

Viewing from near Mt. Hollywood in Griffith Park, look for the ripe red toyon (Christmas) berries in the middle foreground. They tell you that it’s December. But after two heavy rain years, this season started with no rain, leaving the fuels on these slopes dry and primed for ignitions. Those high and middle clouds are drifting from a storm to the north that will never get here. The same resilient high pressure that is compressing the inversion layer (note the haze and smog trapped against the mountains) is blocking potential storms. In a few weeks, these dehydrated Hollywood Hills and the distant San Gabriel Mountain slopes will erupt in flames.
A mix of high clouds above LA’s Griffith Park Observatory in December and January often signal an incoming storm. Not this year. They disappointed us day after day into January.

Next, add autumn’s dry winds. By mid-November, previous gentle offshore breezes occasionally turned to classic Santa Ana winds and red flag warnings, finally sweeping shallow marine layers out to sea. Relative humidity tanked. The Mountain Fire in Camarillo scorched more than 20,000 acres, 200 structures (including homes), and destroyed millions of dollars of agricultural products in early November. By December 9, it still hadn’t rained, encouraging the Franklin Fire to terrorize Malibu all the way to PCH during another gusty Santa Ana wind event. Sadly, these were just dress rehearsals for the big shows.

On January 1, it looked like winter in Eaton Canyon at the base of the San Gabriels. Sycamore trees had changed color, pretending to live in a colder climate. But there should be more water here this time of year. Note the dehydrated soils and vegetation more common to September or October. This is a really bad sign. Just one week later, a devastating wildfire raged off these slopes, destroying everything in its path, including Eaton Canyon’s beloved nature center.

As January progressed, offshore wind episodes became more threatening as the great drying trend expanded across the entire state. By early January, the National Weather Service was warning of dangerous, life-threatening (and possibly historic) Santa Ana winds that would barrel into Southern California on Tuesday, the 7th. Unfortunately, the forecasters nailed it. By Tuesday afternoon, the winds were howling until it seemed as if helicopters were hovering above our homes all night. I’ve written about these devil winds before on this website and in my book and I’ve experienced and researched scores of them over decades, but this was different.

Forecasters at the National Weather Service began warning us days ahead of time that this would be a game-changing Santa Ana wind.

We were caught in a wide, massive atmospheric wind tunnel midway between a low-pressure system dropping to our southeast and a strong high-pressure system trying to assert itself to our west. Upper- and lower-level support grew into an historic pressure gradient that forced cool, stable air masses toward the coast, where they would be warmed by compression. But there was another problem: the mountains were in the way. As the heavy air parcels were pushed up the opposite sides of the mountains, they eventually made it to the top, where they were free to cascade down the coastal slopes toward the ocean to become leeward waves. Widespread gusts were clocked at over 70 mph; a few made it over 90 mph. Meandering mountain waves, chaotic eddies, and violent rotary currents formed downwind of the mountains, spreading over developments, infrastructure, and millions of residents on the coastal plain. Though the powerful winds blew from the continent, wind directions would temporarily jerk one way and then the other without warning as the powerful eddies circulated by. Giant trees and power poles were toppled as power outages swept across Southern California. The big show began to resemble a terrifying scene in a science fiction movie, except you couldn’t write a script that could better prime a landscape for the ignitions that would follow.

Look carefully to see some of the visitors who will enjoy hiking Eaton Canyon for the last time before the big wildfire. There was abundant water here last year at this time, but the stream remains dry into early January, 2025. The canyon last burned more than 30 years earlier, reminding us how these plant communities have adapted to fire. Just as we mourn the unfathomable human losses of the Eaton Fire, we can’t forget how these natural landscapes play such important roles in our physical and mental health.

My chronological photo essay below illustrates how a wildfire can quickly explode into a deadly monster, consuming everything in its path until it meets the ocean. This was the case as our beloved Pacific Palisades natural and human landscapes were destroyed within a few hours this week. Given the conditions I’ve just described, it should also be no surprise that another conflagration would race out of the foothills below the San Gabriel Mountains on the same day. The death and destruction barged into Altadena and Pasadena neighborhoods that seemed far removed from the dangers of what we might consider a wildland-urban interface. (The extend of such imaginary boundaries is being reevaluated.) The greatest surprise may be how heroic firefighters were finally able to stop such an out-of-control train inferno before it did even more damage.  

I’ve experienced and written about too many of these disasters over the years. The ominous red sky, the choking smoke, curious ashes fluttering down to resemble delicate snowflakes, butterfly wings, and rose petals: you may have read about them here or in my book. But I’m one of the lucky ones—so far—as these heartbreaking catastrophes become more common. Admit it or not, we all know what’s going on here. Our relationship with nature has gone seriously awry. We’re testing her and she’s winning and she always will. We’ve got to find better ways to increase our natural history and science literacy and reconnect to the real world or we’re all toast. Without such a paradigm shift, we will continue to feel the potential of the California Dream, and all that we love about our Golden State, slip away. And if you think you can simply escape to other states or countries with greener pastures, take a closer look at the chaos and dysfunction beyond our borders. Maybe if you stick around, you can play your role in righting our ship.

UCLA’s Park Williams and other researchers have teamed up to learn how much of these severe events might be connected to the bigger climate change puzzle. Click here for their most recent article.

Here’s another perspective (slightly compressed) from renowned climatologist Bill Patzert:
“…decades of ‘criminal’ zoning, totally irresponsible building codes, inadequate water storage to deal with fire apocalypses and not dealing with a power delivery system that ignites fires year after year, are the major culprits.” 
Patzert also emphasizes that “global warming is the greatest existential threat to the environment and our civilization, but what we are living through now is human carelessness and ignoring the natural climate forces of Southern California.” But his interview with the LA Times sums up this year: “During my career, I’ve never seen punishing Santa Ana events so overwhelm the normal winter rainy season.”

Regardless, here is where my sign-offs are getting a bit repetitive: keep your seatbelts fastened.

And now follow me as we watch the peculiar behavior of the horrific wildfire that terrorized the Pacific Palisades and changed our world.

From Santa Monica, we could see that a small fire had erupted on a remote ridgetop upwind of Pacific Palisades before 11 am.
The wildfire exploded and grew by the minute. The good news? To invade into Palisades neighborhoods (on the left), it would have to advance downslope, and fires usually burn much faster uphill.
The bad news? It didn’t have to spread downhill. The Santa Ana wind was so strong, it carried and deposited burning embers up to a mile, starting several new spot fires far ahead of the original blaze.
The blaze made noticeable progress within minutes, but responders were prepared. The air battle had already started.
Within an hour, emergency messages were blaring out of our phones and people were gathering to watch the battle. But it quickly became clear that the wind and the wildfire were winning.
Super scooper pilots braved what seemed to be dangerous winds and insurmountable odds. Sirens screamed in the distance as fire crews raced toward the growing inferno. By this time, the accelerating winds were blowing smoke plumes miles out into the Pacific.
We could sense that this fire wouldn’t stop until it reached the ocean after burning through densely populated neighborhoods in its path.
In desperation, fire crews had to focus on threatened neighborhoods while other flanks of the fire quickly spread out into the dry fuel. Some of these plant communities hadn’t burned in more than 40 years.
Watch the super scooper in the distance as it skims over the ocean below the smoke plume, gathering tons of water to be dropped on the advancing flames.
By about 3 pm Pacific Standard Time, Santa Ana winds had already blown the Palisades Fire smoke plume past the Channel Islands (lower center of this image), less than 5 hours after it started. Source: NOAA/National Weather Service.

If you want to experience the drama of escaping the Palisades firestorm and rushing to evacuate, check out Tracy’s series of photos and videos arranged in chronological order as escapees eventually make it down to PCH. The last images show an heroic officer using their hose to douse spot fires started by embers landing in their yard. Note how such a fire can advance with its burning embers through the sky faster than on the ground. (Please appreciate that these images are personal, raw, and unedited.)

Here is a time-lapse video showing the start of the Palisades Fire from another angle from 10:45am – 2:48pm. Thanks to NPS Ranger Susan Teele for sharing.

The advancing fire can be seen here from Santa Monica. Notice how Santa Ana winds are pushing the smoke plume and palm trees toward the ocean. Flames became visible from vantage points across the city.
The Big Blue Bus shows how life goes on during this unimaginable first afternoon of fire. While Pacific Palisades neighborhoods were already being scorched, flanks of the fire would gradually expand until more densely packed urban neighborhoods were threatened. This is the flank that eventually spread several miles east (away from the coast!) into the Brentwood Hills, Mandeville Canyon, over toward the San Fernando Valley, and nearly to the 405 Freeway.
Meanwhile, back at the base of the San Gabriel Mountains around Altadena, during late morning and that same fateful January 7 windstorm … Looking up toward the ridge, a roll of clouds condenses in ascending air and then evaporates in the descending air on the opposite side of the developing wave. That low pressure system dropping into northern Mexico (see weather maps below) was circulating just enough wraparound moisture to make it up to SoCal’s mountain ranges, but not enough to slow the terrifying wildfire that would erupt on these slopes later in the day. Photo by Matt Wright.   




By that evening of January 7, fierce winds fanned sparks generated from near a homeless camp located below high-power lines (both common sources of wildfire ignitions) that spawned the Eaton Fire at the base of the San Gabriel Mountains. The blaze exploded and barreled down the slopes of Eaton Canyon. Blown by powerful winds, the inferno quickly raced into adjacent neighborhoods, destroying more than 9,000 homes, schools, businesses, and houses of worship. At least 17 people didn’t make it out in time. Photo by Matt Wright, just before their home was consumed.

This time-lapse video shows a Mt. Wilson view of the Eaton Fire from January 7-8. Another thanks to NPS Ranger Susan Teele for sharing.

Back in Santa Monica … Offshore winds became so strong during the first two days of fire, they sheared off any smoke clouds that tried to billow higher. Notice (behind Santa Monica Pier) the turbulent eddies and swirls caused by friction and extreme turbulence flowing off of the mountains and out over the ocean. Those lighter high cirrus clouds are not associated with the fire and smoke.
This 500mb map from January 8 illustrates how strong upper-level support helped to generate such powerful winds. Note the tight pressure gradient that has formed over Southern California between high pressure pushing in from the Pacific and deep low pressure that dropped into northern Mexico. Source: NOAA Weather Prediction Center.
Surface map from January 8. A steep surface pressure gradient has also formed over Southern California between strong high pressure to our northeast and deep low pressure to our south, steering damaging winds to flow from the northeast and over us. Source: NOAA Weather Prediction Center.
By the second and third days, unthinkable damage had been done in the Palisades as an eerie sickening veil of smoke settled over the area. Locations downwind continued to be threatened by burning embers. Slight changes in wind directions could have spelled disaster for any one of these neighborhoods.
By the second day, smoke plumes from the Palisades and Eaton Fires (light brown streaks) were swirling in giant eddies hundreds of miles over the Pacific under the strong high pressure that helped generate those powerful winds. More definitive lighter clouds (not related to the fires) and Sierra Nevada snowpacks are also visible. Source: NOAA/National Weather Service.
By day two, crowd control took over and evacuation zones advanced.
Strong Santa Ana winds challenged palm trees up on Palisades Park to stay anchored so they didn’t fly off to the beach. We are looking toward the fires and choking smoke.    
Some of the palms became victims of the vicious windstorm.
Trees and power lines fell across the Southland, blocking roads, while locals talked of winds they have never imagined.
The soil wasn’t even wet. How old do you think this tree was before it became another victim of this historic windstorm?
Residents, workers, and business owners in some of LA’s most iconic districts (such as the Brentwood Village) kept nervous eyes on the advancing blaze and smoke as mandatory evacuations expanded all the way up to San Vicente Blvd. They got lucky this time around, but few ever thought that such danger could visit them here.
Though winds finally began to subside, cautionary Red Flag Warnings extended through the week.  
By Thursday (day three), the Palisades and Eaton Fire smoke plumes were easy to spot on satellite imagery as they spread out over the Channel Islands and beyond. Source: NOAA/National Weather Service.
As if we hadn’t had enough, this Santa Ana wind and fire story was far from over when the National Weather Service issued these warnings for January 11-15. Rain dance anyone?
SoCal, we have a problem. Because data for this map starts on October 1 (our official water year), it doesn’t even show how this exceptionally dry period followed our summer dry season (since spring), which was also dryer and hotter than average. We’re now in our 9th straight month of prolonged dryness. Northern Cal already benefited from a very wet start to their rainy season (see our previous story on this website), so no drought problems—yet—there. Source: Weather West.

Notice how above-average precipitation quickly dwindles to far below average for this season as we move from Northern California to Southern California weather stations: https://ggweather.com/seasonal_rain.htm

When do California’s playgrounds become forbidden land? Storied Pacific Coast Highway toward Malibu was closed to everyone except emergency vehicles. Fortified National Guard barriers helped to seal the evacuation zones. This is at the famed California Incline.    
It’s only 5 days after the cataclysm broke out, but most of the Palisades Fire has been reduced to a smolder. Compare this to the earlier view toward Santa Monica Pier (as the fire raged). Here, a welcome breeze out of the southeast pushed the smoke away, yielding relatively clear, blue skies. But the surfers who were riding gentle waves appear as absurdities when you look closely at hillslopes in the background. The formerly dark and light greenish-gray coastal sage, chaparral, and human settlements built in between have been charred into burnt remnants of the before times, all the way from Malibu to Mandeville.
Over many years, I’ve seen these signs erupt in too many communities in nearly every region across the western US. Few would have ever guessed this could happen along Santa Monica’s posh Montana Avenue shopping district, as it was precariously positioned on the evacuation boundary zone. Let’s hope this show is not coming to a community near you.      

This NY Times article supports Bill Patzert’s earlier comments.

Check out this NY Times Article: Researchers show how Santa Ana wind speed is the main variable that makes SoCal fires more destructive.

This research is from the International Journal of Wildland Fire: Climate and weather drivers in southern California Santa Ana Wind and non-Santa Wind fires

Santa Ana wind history and trends.

THE END??? All the stories on this website and in my California Sky Watcher book confirm what we’ve learned from experience: nature’s cycles never “end” and we’re just a part of them. Should it finally start raining in SoCal, the next chapters will likely feature catastrophic mud and debris flows that always follow these fires after they have stripped the covers off our hillsides. Stay tuned!

The Unimaginable Epilogue

Dominant upper-level high-pressure systems settled over the entire West Coast and generated exceptionally dry on-and-off offshore wind events across California for more than two weeks after the worst wildfires started. In Southern California, powerful Santa Ana winds howled through January 23, fanning numerous new fires just as crews tried to mop up some of the most destructive wildfires in California history. Relative humidity dropped into single digits throughout SoCal. But finally, for the first time since spring, weather forecasters were tracking a low-pressure system capable of delivering precipitation that promised to be the final blow to the fires by January 26. This little system wouldn’t direct any atmospheric rivers over the fire scars. We will have to wait to see if those will arrive during our other normally wet months of February and March. To learn more about the science and power of atmospheric rivers, you might check out my story about ARs on this website or read my feature article in the current edition of Weatherwise Magazine.          

This 500mb map from January 22 shows the high-amplitude upper-level waves responsible for record-breaking January weather across the US. This resilient pattern remained stuck in place for several days. Following the pressure heights, you can see winds curving up and over that elongated high that dominated over the West Coast. The cold air then dropped down on the east side of the high and into the Great Basin, further enhancing strong offshore pressure gradients over Southern California. (Such exceptionally cold air masses also help explain why so many of this season’s Santa Ana winds felt “cool” even after the compressional heating.) Now follow those upper-level winds as they blast out of northern Canada and dip into the deep trough directly into the Midwest and southern states, carrying snow and a memorable deep freeze all the way down to the Gulf Coast. We can see how California’s record dry fire weather and the arctic blasts to our east were connected, all powered by these upper-level pressure patterns. Source: NOAA Weather Prediction Center.
Strong high pressure keeps the entire West Coast mostly clear on January 23, 2025. It was just another day in the series of dry, gusty offshore wind events that dominated through most of the month. The winds blow two large smoke plumes into the Pacific from the latest wildfires in northern Baja California. Source: NOAA/National Weather Service.

Here are three videos shared by Karin from the Topanga Canyon Docents:

Topanga resident Elena Roche made a number of videos during the fire. You can see more on her YouTube site. Here, active fires were blocked just before they could burn through the community of Topanga and parts of Trippet Ranch. By this time, the fire fronts were spreading several miles around after ravaging the Pacific Palisades.

This video takes you up from PCH through Topanga Canyon in the aftermath to see what burned and what escaped the flames, and why any substantial rain will produce destructive mud and debris flows. It was filmed on January 17th.

Here are personal stories from the Topanga New Times published just before the first rain finally came.

The documentary Dry Times, made by Anurag Kumar and Alex Gregory, has, unfortunately, become more relevant as it captured California’s recurring predicaments during the megadrought that spanned more than two decades: Given recent events, this has become a haunting trailer. The Movie

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Precipitation Extremes in a Bipolar California https://rediscoveringthegoldenstate.com/precipitation-extremes-in-a-bipolar-california/?utm_source=rss&utm_medium=rss&utm_campaign=precipitation-extremes-in-a-bipolar-california Sat, 11 Jan 2025 09:12:31 +0000 https://rediscoveringthegoldenstate.com/?p=4754 How can one state simultaneously experience more than two months of soaking storms and floods AND desiccating drought and wildfires? Here’s a story about stubborn weather patterns that divided...

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How can one state simultaneously experience more than two months of soaking storms and floods AND desiccating drought and wildfires? Here’s a story about stubborn weather patterns that divided California in half and refused to budge. Part Two (see page 2) explores recent research from the scientists who are trying to explain these recurring weather whiplash anomalies.

We are viewing toward the west as one of the late November, 2024 storms was already drenching Northern California and began moving over the San Joaquin Valley here near the Grapevine. But like so many others this season, this potential drought buster would fade before making it past the Transverse Ranges and into Southern California. Photo by Matt Wright.
The same storm looks promising as it approaches the San Joaquin valley near Interstate 5, but we’ve reached this season’s dividing line between the wet north and dry south. Photo by Matt Wright.

We frequently highlight the startling contrasts between the relatively wet slopes and valleys facing the Pacific (cismontane California) versus our true deserts on the continental rain shadow (transmontane) sides of California’s major mountain ranges. Since this is NOT our focus here, you can surf back into our website or check my book to find those stories. In most years, a more gradual transition usually develops between wetter Northern California (closer to the path of winter’s storms) and relatively drier SoCal (where resilient high pressure often veers storm tracks to the north). But as 2024 evolved into 2025, that annual pattern became historically dramatic, as if the ancient mythological Mediterranean Gods Zeus or Jupiter had conspired with Mother Nature to build a massive wall between north and south.

This water vapor image (on November 20, 2024) shows a strong middle latitude cyclone spinning west of Vancouver, extending a weather front and atmospheric river south into Northern California. Southern California remained dry. Source: NOAA/National Weather Service.
On November 20, 2024, a potent early-season atmospheric river barreled into the Pacific Northwest and Northern California, helping to flood any remnants of a fire season there. But blocking high pressure kept Southern California clear and warm, setting the stage for fire catastrophes in the months ahead. Source: NOAA/National Weather Service.
Here’s what the big “bomb cyclone” looked like on surface weather maps as it churned off the Pacific Northwest coast on November 20, 2024, Note the frontal system extending rain into Northern California, while stubborn high pressure guards Southern California. Source: NOAA Weather Prediction Center.

Winter’s rainy season roared in early like a lion in the north, renewing concerns about flooding. But the storms were no-shows in the south, extending summer’s drought and fire season well into the new year. California’s fickle bipolar weather patterns developed in November and December, 2024 and expanded into January. Jet streams, storm tracks, and soaking atmospheric rivers raced off the North Pacific and made their annual gradual migrations into the Pacific Northwest and toward Northern California early in the season. But by the time they crept farther south into Central California, they encountered unseasonably resilient high-pressure ridges that blocked their progress so that storms were instead ejected north and east, leaving Southern California dry under the high.

By November 20, storm clouds were breaking over San Francisco after delivering precious rainfall. Photo by Matt Wright.
Various cloud formations drift with the west winds and follow a frontal system through the Golden Gate on November 20. Photo by Matt Wright.

Late autumn and early winter’s exceptional meteorological boundary between wet Northern and dry Southern California could be drawn roughly along a line from the central coast near Big Sur, then east across the San Joaquin Valley and southern Sierra Nevada. Locations far north of this line, especially up past the Bay Area and near the Oregon Border, were getting clobbered by powerful winter storms that included classic atmospheric river deluges. When an early-season atmospheric river barreled through Northern California and targeted Sonoma County in November, 2024, several weather stations recorded more than one foot of rain in less than three days. But the storms couldn’t penetrate into resistant high pressure that dominated south of our imaginary boundary. From November well into January and the traditional rainy season, weather fronts repeatedly died out as they approached and then navigated the Transverse Ranges, particularly south of Santa Barbara.

As 2024 came to a close, persistent weather forecasts included rain for several consecutive days and even weeks in the north, but fair and dry weather in the south. Though we expect Northern California to easily win in the annual rainy season water wars, this season’s abnormal pattern seemed to be on steroids. By the start of 2025, seasonal rainfall totals (in the three+ months since Oct. 1) ranged from more than 50 inches on Pacific slopes near the Oregon Border to widespread totals of less than 0.25 inches along the Southern California coast. Located on those wet Pacific slopes near Oregon, Gasquet recorded more than 125 inches of rain for the 2024 calendar year, while some SoCal coastal weather stations had accumulated around 1/10th of an inch since the last spring! Weather headlines on the northwest coast emphasized flood stages on local streams and rivers while residents of the south coast were warned of dangerous drought, red flag warnings, and wildfire conditions that threatened well into January.

Storm waves and heavy rains battered our north coast and even caused some damage through December, 2024. Thanks to Laurene von Klan.

As if to demand attention, descending air from the resilient high pressure over SoCal was heated by compression to produce widespread temperatures over 80°F in the coastal plains and inland valleys. Here are some example high temperatures on December 18: Oxnard, 87; Ventura, 85; Santa Monica, 82; Santa Barbara, Los Angeles, Long Beach, Pasadena, and Santa Ana all made it to 83°F before that stable and stubborn marine layer reinvaded immediate coastal strips. Mountain resorts (such as the Big Bear station at 6,752’) measured record high temperatures for the middle of December, well into the 60s. Between dry Santa Ana wind events down south, the NWS forecast grew ominous as we approached the middle of our precious rainy season: “… longer range ensemble solutions continue to offer few if any signs for additional rain through at least the middle of January.” That’s when high pressure built over the entire state and at least briefly cut off rain even to the north into mid-January, producing a series of powerful Santa Ana wind events that would fan catastrophic firestorms across Southern California.           

Typical of the late autumn and early winter of 2024, another frontal system approaches Northern California, but will miss Southern California, as shown in this December 19 satellite image. Note the dense, stable valley (tule) fog that has settled in the Central Valley after surfaces were dampened by previous storms. Source: NOAA/National Weather Service.    
Weather patterns began to change during early January, 2025. This 500mb map (halfway through our atmosphere) shows a massive upper-level high pressure system starting to build off Southern California. As it expanded, the storm track was directed farther north, guiding disturbances north of California and then dropping them down into the Great Basin and middle of the continent (note the low-pressure trough to our east). The entire state began drying out while offshore surface winds would develop into powerful Santa Ana conditions in the south, where a ridiculously dry season became even dryer. Source: NOAA Weather Prediction Center.

As this story is published, no one knows what to expect in the long term during a weak La Niña year in such a climate of change, but precipitation patterns along the West Coast so far are more characteristic of stronger La Niña years. And as if to mock the regional anomalies, official measurements of water content in the Central Sierra Nevada snowpack were near average by January 1, masking the remarkable contrast between the wet north and dry south. Here’s yet another example of how more widespread and equally-distributed beneficial precipitation has become the exception to the more common extremes we have recently experienced across the state. So, what is going on? Click on to Part Two (Page 2) to learn what scientists are discovering and keep your seat belt fastened. 

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October Temperature Extremes in a Climate of Change https://rediscoveringthegoldenstate.com/october-temperature-extremes-in-a-climate-of-change/?utm_source=rss&utm_medium=rss&utm_campaign=october-temperature-extremes-in-a-climate-of-change https://rediscoveringthegoldenstate.com/october-temperature-extremes-in-a-climate-of-change/#comments Thu, 12 Dec 2024 08:17:50 +0000 https://rediscoveringthegoldenstate.com/?p=4709 Another round of record-setting weather patterns swept across California as September yielded to October, 2024. In page one of this story, we follow these atmospheric anomalies and investigate their...

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Another round of record-setting weather patterns swept across California as September yielded to October, 2024. In page one of this story, we follow these atmospheric anomalies and investigate their causes. Then, in page two, we explore (highlighting a recent National Weather Service workshop) how climate change looms in the background, creating a challenging atmosphere of uncertainty. (In a future story, we will explore Northern California’s November atmospheric river, southern California’s destructive wildfires, and other autumn, 2024 weather whiplashes that will live in the history books.)

Breaking October Records

Autumn is usually the season when dense high pressure builds over cooling land surfaces in the Great Basin. This annual reversal in temperature gradients also helps to reverse the onshore pressure gradients that pushed sea breezes and marine layers inland during the long high sun season. In contrast to summer, autumn brings those offshore winds that howl off the continent and toward the coast, occasionally shoving summer’s moist ocean air masses far out to sea. As the continent cools further, these descending offshore winds are often compressed to produce some of the warmest and driest days of the year for immediate coastal strips from Oregon to Mexico. You will find detailed accounts of these seasonal turnabouts in previous stories (such as our Offshore Autumn) on this website. But in 2024, some unprecedented early autumn glitches developed as September progressed into October.

This 500 mb map shows an unusually deep upper-level low-pressure trough digging south over California. It sent a cold front with high surface winds that churned up cold waters from the depths all the way along the Southern California coast. The early low pressure would eventually be followed by strong high pressure that orchestrated record-breaking heat waves across the state well into October. Source: National Centers for Environmental Prediction, Weather Prediction Center. 

The first surprise was an early season Pacific Northwest storm that dragged a dry cold front down the coast in mid-September. High winds following that system churned up coastal currents, quickly dropping Golden State water temperatures by several degrees. For instance, Santa Monica Bay water temperatures that had just spiked near 72° F plummeted at least 7 degrees, down below 65° in just two days. Water temperatures wouldn’t recover, forcing an early end to my comfortable summer swims without a wetsuit. A premature Southern California coastal chill was suddenly noticeable in the daily sea breezes, which often ebbed below their dewpoints, causing the air to remain saturated for longer periods spanning several straight days. (Some NWS forecasters have postulated that the threshold water temperature, helping to determine whether or not summer marine layers are saturated with fog and low clouds as they drift onshore, is around 68°F.) Along the Southern California Bight, stubborn fog and low clouds condensed over the cold water and hugged the immediate coast into October as if May gray or June gloom conditions forgot to check the calendar, while the expected seasonal offshore wind trends were not strong enough to shove the shallow misty muck all the way out to sea. 

Dried yucca stalks pepper the chaparral and coastal sage scrub during autumn. They were blooming through the traditional May gray and June gloom seasons. This one looks down toward the ocean from the Santa Monica Mountains, into the strip of coastal fog that is more typical of late spring and early summer. Descending air masses out of upper-level high pressure clamped a lid on the shallow fog, but weren’t strong enough to push the marine layer out to sea.     
As inland regions (behind us) cook in record heat, the shallow, cold fog is trapped below descending air from strong high pressure. Surface air remains saturated above ocean temperatures that prematurely plummeted in mid-September, resulting in these scenes more typical of May and June along the immediate coastal strips. The cascading fog can only attempt to penetrate farther inland. 

Just several miles inland, and throughout parts of Northern and Central California, it was a radically different weather story. Some of the strongest high-pressure domes on record for the dates anchored directly over the state and into other southwestern states. As the calendar flipped from September to October, a prolonged and dangerous heat wave intensified. Air columns were compressed and superheated to break numerous daily records until several inland stations recorded their all-time highest temperatures for the month of October. As is often the case in autumn, the offshore trends occasionally swept all the way to the beaches in parts of Northern and Central California. Intense heating of the brilliantly clear dry air pushed temperatures over 90° F in San Francisco and 100° F slightly farther inland, from Santa Rosa to San Jose. Exemplifying those rare warm San Franciscan nights, surrounding Bay Area hills recorded overnight low temperatures well over 80° F beneath the descending air columns. More high temperature records were broken in the Central Valley. Back down in Southern California, the stage was set with conditions that produced some of the most extreme temperature gradients (across such short distances) on the planet.    

This 500mb map shows a massive, powerful dome of upper-level high pressure over California and the southwest on October 1. Descending air out of this dominant system was responsible for consecutive days of record high temperatures. Source: National Centers for Environmental Prediction, Weather Prediction Center.
By October 2, surface high pressure continued to dominate across southwestern states, supported by that upper-level high illustrated on the previous map. Thermal lows were locally forming in the super-heated air near the surface. Source: National Centers for Environmental Prediction, Weather Prediction Center.
By October 3, a sprawling upper-level high continued to dominate across California and the southwest. Descending air masses baked inland regions, extending a brutal summer well into October. Source: National Centers for Environmental Prediction, Weather Prediction Center.

Epic Southern California Temperature Gradients

As high pressure strengthened directly overhead, numerous daily records (and some all-time October records) were also broken in Southern California’s deserts and inland valleys (see the list near the end of this story). Indio and Palm Springs made it to 117° F, their hottest temperatures ever recorded for October. On October 6, it got up to 116° in Indio, which is the hottest it’s ever been so late in the year anywhere in California. Exceptional high-desert temperatures repeatedly exceeded 100° F in early October and inland valleys were even hotter. Paso Robles hit 107° and Woodland Hills (in the western San Fernando Valley) topped out at 113° F. And in contrast to the annual cooler Great Basin High common to autumn, these hot high-pressure domes formed right overhead. So, instead of generating strong offshore winds typical of October, they compressed gentler breezes that couldn’t make it to the surface along the immediate Southern California coast.

This resulted in unseasonal temperature gradients that would have been remarkable even for June and July. For instance, on the afternoon of October 1, it was 67° F in Oceanside when it was 117° in Palm Springs, less than 70 straight line miles and a few mountain barriers inland. On October 2, when it was 71° F along PCH in Malibu, it was a sizzling 111° in Woodland Hills, less than 10 miles and a small mountain range away. Imagine such a temperature gradient of more than 4 degrees/mile! Folks who headed to the beach to escape record inland heat were astounded when they were met with a wall of shallow cold fog that drifted along the beaches and only several blocks inland during the day, and then crept only a few miles farther inland at night: June- and July-style heat waves (as featured in an earlier website story) trending into October. By late October, inland temperatures were mercifully moderating, though persistent high pressure continued to clamp a lid on the stubborn shallow marine layer that was attempting to creep in below it. By the time the Dodgers were beating the Yankees in the first two games of the World Series, a packed Dodger Stadium crowd had a clear view looking inland toward the warm mountains, while a distant hazy marine layer loomed toward the coast. It was the kind of perfect Southern California baseball weather that can make national audiences envious, another interesting topic in my California Sky Watcher book.    

On this October 3 satellite image, notice how seasonal offshore flow was plenty strong enough to push the marine layer out to sea in Northern California, so that hot and dry conditions extended all the way down the Central Coast. But the land breezes weren’t strong enough to scour out the shallow fog and low clouds that hovered at the surface over unseasonably cold waters in the Southern California Bight … all the way down the Baja coast. An eddy of shallow cold fog enshrouded Southern California beaches while inland locations continued setting high temperature records. Source: NOAA/National Weather Service.
By October 5, a surge of misty cold marine layer fog and low clouds crept north up the Central Coast, more reminiscent of May gray and June gloom. But the string of high temperature records continued inland across the southwest states, as they were stuck below that high pressure dome. Source: NOAA/National Weather Service. 
On October 6, Huntington Beach was smothered in the shallow coastal fog while inland valleys and deserts continued to sizzle. This disappointed crowd came to observe the annual Pacific Airshow, which is almost guaranteed clear and sunny afternoons this time of year, after summer marine layers have burned off and before winter’s rainy season turbulence. October 2024 was a strange and chilly exception to the seasonal rule at the storied pier.     
Most visitors from afar had escaped record inland heat to see the Pacific Airshow in Huntington Beach in 2024. Instead of normally sunny early October afternoons, they were surprised to meet the enshrouding fog here at Huntington Beach Pier. There were no refunds for those who invested in tickets ahead of time to get their close-up narrations. The event evolved into an unseasonably awkward no-fly zone no show.

Though every heat wave has its own personality, these recent record busters followed a trend that has become all too familiar in California and the Southwest U.S.: while all weather stations are showing signs of warming, inland locations are heating up faster. This is likely due to the modifying effects of ocean breezes that dominate our coastal regions but don’t penetrate far enough inland, resulting in slower warming along the immediate coast and enhanced temperature gradients toward super-heated inland regions. And this leads us into Part Two of this heated discussion. If you are interested in what lurks behind all the wild weather whiplash and record temperature extremes that are threatening and remaking our Golden State, click on to Page Two of this story. You might first want to surf down the list (below) of some remarkably high temperatures recorded during our historic 2024 October heatwave and then see what weather patterns finally broke the heat spell.                 

Afternoon of Oct 1:
Oceanside: 67°F versus 117°F less than 70 miles east in Palm Springs (record for October).

Afternoon of Oct 2:
Topanga/Malibu coast: 71°F versus 111°F less than 10 miles inland in Woodland Hills (record).

Here are examples of early October, 2024 high temperatures (in F degrees) recorded at selected weather stations in California, with some comparisons to previous records:

  • Campo: 105 degrees.
  • Hanford: 100, breaking the prior record of 98.
  • Idyllwild: 98, breaking the prior record of 93.
  • Indio: 117, breaking the prior record of 111.
  • Kentfield: 100, breaking the prior record of 97.
  • Lake Cuyamaca: 94, breaking the prior record of 89.
  • Lancaster: 103, breaking the prior record of 100.
  • Madera, 100, breaking the prior record of 99.
  • Palmdale Airport: 104, breaking the prior record of 100.
  • Palm Springs: 117, highest ever for October (116 in 1980).
  • Palomar Mountain: 93.
  • Paso Robles Airport: 107, breaking the prior record of 106.
  • San Jacinto: 106, breaking the prior record of 105.
  • San Rafael: 105, breaking the prior record of 104.
  • San Jose: 100, breaking the prior record of 97.
  • Sandberg: 95, breaking the prior record of 92.
  • Stockton Airport: 101.
  • Woodland Hills: 113, breaking the prior record of 110.

Before clicking on to Page 2 to review climate change trends (from that National Weather Service workshop), you might check out the following weather patterns that finally broke through the high-pressure domes and heat waves as we made our way through October, 2024.

Breaking the Heat Wave

Even the most stubborn and historic weather patterns must come to an end, and so it was for the unprecedented summer that bled into October 2024. The following images illustrate how California weather finally shifted to what we might expect in autumn.

This October 16, 2024 water vapor image shows an early-season low pressure system finally moving through Northern California and just clipping Southern California. High pressure domes have been shoved aside, marking an end to the historic prolonged California and southwestern states heat waves of 2024. Source: NOAA/National Weather Service.
The October 16 visible image reveals a weak storm spinning across Northern California and a very thick marine layer pushing into Southern California’s inland valleys. Record high pressure and heat retreated into the rear-view mirror. Source: NOAA/National Weather Service.
By October 18, a deep upper-level cutoff low/inside slider (as shown on this 500mb map) had dropped just east of California. This upper-level pattern may be more characteristic of autumn and is diametrically opposite from the anomalous high pressure and inland heat earlier in the month. Also note how such amplified upper-level waves often produce contrasting weather conditions between eastern versus western sides of the continent. Source: National Centers for Environmental Prediction, Weather Prediction Center.
By October 27, remnant moisture (seen in this water vapor image) from a dissipated tropical storm was being pulled from southwest to northeast into California. This is a familiar pattern during this time of year, when the warm-season’s last Pacific tropical storms might interact with low pressure troughs that begin to drop south, circulating the moisture ahead, and announcing that winter’s rainy season is not far away. Source: NOAA/National Weather Service.  
This October 29, 2024 surface map shows a weak low pressure and frontal system drifting east after sweeping through California. The big highs and heat waves are memories. Source: National Centers for Environmental Prediction, Weather Prediction Center.
Here is what remains from a dead tropical storm on Oct 27. Various forms of cirrus, altocumulus, and altostratus clouds decorated the skies as they were drawn across the Pacific and onshore by low pressure sagging down from our north. They were a welcome sight in a state seared by those summer heat waves and plagued by SoCal coastal fog that dragged on through early October. But an unstable trigger in the upper levels never got far enough south to wring this moisture out. Southern California would remain mostly dry well into December.
Though early rains didn’t make it this far south, the skies over California were looking more changeable by Oct 27. Weak low-pressure troughs and eye-catching cloud formations (such as the high streaks of cirrus and darker altocumulus here) streamed overhead in the cooler air masses, confirming that the big heat domes were memories in the history books.
Natural and cultural signs of the changing seasons. High and middle-level clouds decorated late October skies at the big annual Dia de los Muertos Festival in Downey. Could the spooky Halloween season cloud backgrounds be harbingers of the historic atmospheric river that would hit Northern California in November?  
By October 28, weak low-pressure troughs and weather fronts had swept through the state, leaving stratocumulus to drift up and over the mountains with the cool breezes off the Pacific. What a contrast to the powerful persistent high pressure that dominated earlier in the month!
Another deep, cold upper-level low pressure trough dug east of California and over the southwest states by the end of October. It looked a lot like the system from just 11 days earlier (and what we might expect in October), bringing more cold air down from the north. Inland and desert regions that had baked at the start of the month were now freezing in nature’s autumn refrigerator. Once again, note how high pressure and warm weather dominated eastern states that were stuck beneath a ridge within such high-amplitude upper-level waves. Source: National Centers for Environmental Prediction, Weather Prediction Center.
By October 30, strong middle latitude cyclones, more typical of winter’s stormy season, were already bearing down on the Pacific Northwest. The first storms barely clipped Northern California (notice the cold front just approaching the coast) and weakened as they moved south. They eventually strengthened and inched farther south until a powerful atmospheric river made landfall north of the Bay Area in November. Southern California missed out on all the early storm drama only to suffer devastating wildfires into December. Such extreme precipitation events will be highlighted in our next story on this website. Source: NOAA/National Weather Service.

If you are interested in reviewing some of the trends (with help from a National Weather Service workshop) that might help to explain these autumn records, click on to Page 2 of this story. At the end, you will also find a long list of links that dive into climate change trends in California and how we are measuring and dealing with extreme heat events. You can start with the following image:

SOURCES: Statewide temperature raster data for the period 2024–2100 from downscaled general circulation models (GCM) were published by the Scripps Institution of Oceanography and obtained from Cal-Adapt. Historical observed temperature data for the period 1950–2023 were obtained from the Western Regional Climate Center.
NOTES: Historical observed temperature data are shown for the period 1950–2023. Data derived from the output of downscaled GCMs (e.g., climate model data) are shown for the period 2024–2100. The moderate emissions scenario is RCP4.5 and the high emissions scenario is RCP8.5. These downscaled GCM data were originally published in California’s Fourth Climate Change Assessment as annual maximum and minimum temperature time series. For further details, see the source notes to this brief.

The image above shows historical and projected California temperature trends as shown in PPIC’s Priorities for California’s Water .

Click to Page 2 for Researching Heat Risks and Heat Wave Trends with the National Weather Service.

   

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