Underground Fury: The 1985 Methane Blast That Rocked Los Angeles and Rerouted Its Subways

A 1985 methane explosion in L.A.’s Fairfax district turned a Ross Dress for Less into a disaster scene.
Photo by Dean Musgrove, courtesy of the Herald-Examiner Collection – Los Angeles Public Library.

In the heart of Los Angeles, on a seemingly ordinary spring day in 1985, a sudden explosion tore through the Ross Dress for Less store at the corner of 3rd Street and Fairfax Avenue. This wasn’t an industrial accident nor was it an act of malice—it was a force of nature that had been lurking unseen beneath the city’s streets: methane gas.

The Fairfax District, a bustling area known for its shopping and historic Farmers Market, is also part of the larger Salt Lake Oil Field, a subterranean landscape rich in hydrocarbons. Over millions of years, decaying organic matter trapped in the earth’s crust had transformed into vast reservoirs of oil and methane gas. It was this methane that had stealthily migrated close to the surface, building up in closed spaces, waiting for an ignition source to set off a dramatic release.

On that day, as shoppers browsed through discounted apparel, an explosive mixture of methane, oxygen, and sewer gases found its spark. The blast shattered the storefront windows and caused a partial cave-in of the roof, turning the shop’s interior into a mangled wreck of metal debris. Twenty-three individuals were left with injuries severe enough to necessitate hospital care. In the aftermath, police cordoned off a four-block radius encompassing the bizarre spectacle of gas fires that jetted into the night sky, a haunting tableau that persisted until dawn.

The aftermath of the explosion was a scene of chaos and confusion. Emergency services sprang into action, addressing the immediate humanitarian concerns. But once the dust settled, a more profound issue loomed: the implications for the city’s ambitious underground Metro Rail project.

At the time, Los Angeles was in the throes of planning and constructing the Metro Red Line, a subway system that promised to link various parts of the sprawling city. Wilshire Boulevard, one of the busiest thoroughfares in Los Angeles, was to be a central artery in this new subterranean network. However, the explosion at Ross Dress for Less exposed the heretofore underestimated risk of tunneling through methane-rich zones.

The city of Los Angeles created a methane zone map showing shaded regions of the methane zone and methane buffer zones.

Fears quickly escalated about the potential for similar explosions occurring elsewhere, particularly along the planned subway routes. The public, already wary of the high costs and disruptions associated with the Metro line, grew increasingly concerned about the dangers of tunneling through methane pockets.

In the wake of the explosion, city officials and Metro Rail engineers faced a daunting challenge. They needed to ensure public safety without derailing the critical infrastructure project. This task required a multifaceted approach. First, there was a thorough scientific investigation. Experts from various fields, including geologists, engineers, and safety specialists, were brought in to assess the risks of methane gas in the Fairfax District and along the proposed Metro route.

In a comprehensive regulatory response, the city imposed stringent building codes and established the Methane Zone Ordinance, which required new constructions in certain areas to implement gas detection and venting systems.

But the blast also resulted in a measure of technological innovation. The Metro Rail project incorporated state-of-the-art methane detection systems and emergency ventilation procedures in its design, setting a new standard for subway safety. The process was aided to some extent by significant community engagement. Public meetings and forums were held to address community concerns, offer reassurances, and provide education on the measures being taken to prevent future incidents.

B Line train at Union Station (Wikipedia)

Despite these efforts, the fear of what lay beneath Los Angeles’ streets had a chilling effect on the Metro’s progress. The Red Line faced delays as policymakers and the public grappled with the cost and complexity of making the subway safe. It wasn’t until the early 2000s, with the introduction of advanced tunneling technologies and robust safety protocols, that the Metro expansion regained momentum.

The 1985 methane explosion, while a localized event, reverberated through time to shape the development of Los Angeles in profound ways. It brought to the forefront the invisible risks of urban growth, challenged engineers and city planners to innovate, and ultimately reaffirmed the resilience of a city determined to rise above its subterranean challenges.

1983 rendering for the planned subway station at Wilshire and Fairfax – a casualty of the Ross explosion.
\Courtesy of the Metro Transportation Library and Archive.

The dangers of methane beneath Los Angeles are far from gone. The Porter Ranch leak, also known as the Aliso Canyon gas leak, was a massive methane leak in the Santa Susana Mountains near the neighborhood of Porter Ranch in the northwest section of the San Fernando Valley.. Discovered on October 23, 2015, gas was discovered escaping from a well within the Aliso Canyon underground storage facility. On January 6, 2016, Governor Jerry Brown issued a state of emergency, and numerous media reports suggested that the methane could be dangerous to residents. On February 11, the gas company reported that it had the leak under control, and finally on February 18, state officials announced that the leak was permanently plugged. Still, an estimated 97,100 tonnes (95,600 long tons; 107,000 short tons) of methane and 7,300 tonnes (7,200 long tons; 8,000 short tons) of ethane were released into the atmosphere.

Today, as the Los Angeles Metro continues to expand, the lessons learned from that explosive day in 1985 continue to resonate, ensuring that safety remains at the core of the city’s march toward the future.

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Journey to the Iron Giant: NASA’s Psyche Mission Could Unlock the Secrets of a Metallic World

The Psyche spacecraft in the clean room of the Jet Propulsion Laboratory in La Canada Flintridge, CA

A NOVEL PROPULSION SYSTEM WILL TAKE US TO A MASSIVE METAL ASTEROID IN DEEP SPACE

Imagine being able to move your car with your breath. One long blow out the back window, and your car begins speeding down the highway. Now imagine that if you keep blowing, your car accelerates to over 124,000 miles per hour.

Of course, if you actually did this on Earth, you would turn blue in the face and your car would remain still. But in the vast vacuum of empty space where there is little gravity and no atmospheric drag, that tiny amount of thrust can be very effective.

On October 12, NASA’s Jet Propulsion Laboratory in La Cañada Flintridge will launch a spacecraft toward Mars and Saturn that will put this idea to the test. The agency is sending a 3,600-pound vehicle into space propelled by futuristic solar electric thrusters that deliver a force equivalent to the mass of about two quarters. They also happen to emit a cool blue glow that looks like something out of Blade Runner.

The Hall Thruster’s eerie blue glow is due to it’s emission of Xenon gas

The spacecraft, called Psyche, launched aboard a SpaceX Falcon Heavy rocket from the historic Launch Complex 39 at NASA’s Kennedy Space Center. The spacecraft will initially be set on a trajectory to fly by Mars, where it will receive a gravity assist, catapulting it further out into the solar system. In late 2026, the spacecraft will enter into orbit around a rare metal asteroid called Psyche 16 (hence the spacecraft’s name). The journey to the asteroid will take over three and a half years and cover over 1.5 billion miles.

Perhaps the most intriguing — and ultimately beneficial — components of the Psyche mission will be its use of solar electric thrusters. Also known as Hall Effect thrusters, the novel propellant system was designed to be efficient and cost-effective. Solar energy will be generated from a five-panel, cross-shaped solar array that will unfold and immediately begin harvesting energy from the sun. At 800 square feet, they are the largest panels ever installed at JPL, and when fully deployed, will extend about the area of a singles tennis court.

The resulting energy will be used to turn xenon, a dense, colorless, odorless noble gas into xenon ions, atoms that carry a charge because the number of electrons does not equal the number of protons. Xenon is found in Earth’s atmosphere in trace amounts and is used in car headlights and plasma TVs. As the xenon ions are accelerated out of the thruster, they create thrust, propelling the spacecraft forward. The amount of thrust, however, will be minuscule compared to that of chemical-based propulsion systems normally employed on missions like those to Mars, Jupiter, and Saturn.

”They operate at a low thrust level,” says David Oh, Psyche’s project system engineering manager. “You can’t use it to launch from the earth. But in space, you operate these thrusters over a long period of time and you can get to very high speeds.”

Psyche spacecraft inside the NASA JPL clean room (Erik Olsen)

In other words, in space, a force equivalent to a hastily expelled deep breath is enough to move a ton and a half of metal through space at a speed more than one hundred times that of a fired bullet.

Psyche will carry over 1000 kilograms of xenon in its tanks, more than enough to get the spacecraft to Psyche and complete its 21-month mission. JPL engineers estimate that the spacecraft would burn through about 15 times that amount of propellant by weight if it had to use traditional chemical thrusters.

“We did try conventional chemical propulsion, and we determined if we did that, we would have quadrupled the mass of the spacecraft. It would have been very difficult to launch and very expensive to build. But this technology was mature and ready to go,” says Oh.

This is not the first time an ion propulsion system has been used in space. Communication satellites orbiting the earth use them regularly. Colorado-based company Maxar Technologies developed and built the Hall thrusters for near-earth orbit, and NASA has purchased them from the company and made some modifications, but this will be the first time they will be used to venture into deep space.

“We needed advanced propulsion to get into orbit. We were looking at what could we buy rather than building our own thruster from scratch,” says Oh.

Because they’re so efficient, Psyche’s Hall thrusters can operate nearly nonstop for years without running out of fuel, says Oh. When its mission is over, the spacecraft might have lots of fuel left over, and they will have to decide whether to find other puzzles to solve. If the mission proves a success, Psyche’s Hall thrusters could play a major role in propelling future missions into deep space.

A Metal Asteroid?

Scientists are giddy at what they might find once Psyche, propelled by the Hall Thruster system, arrives at the asteroid.

“It’s a kind of world that humans have never visited before,” says Arizona State University’s Lindy Elkins-Tanton, principal investigator in charge of the mission. “Most of the exploration we do is going and learning more about a body we’ve already visited. Psyche, we have no photos of it, no one has ever done a flyby or really studied it. It’s unlike every asteroid we know, as far as we can tell.”

Astronomers have been aware of Psyche’s existence ever since since it was first discovered on March 17, 1852, by the Italian astronomer Annibale de Gasparis. The asteroid, computer models of which resemble a potato, was named after the Greek mythological figure Psyche, the goddess of the soul. It is the largest and most massive of the known M-type asteroids (M stands for metal), and is one of a dozen of the most massive objects in the asteroid belt between Mars and Saturn.

Scientists believe that Psyche may be part of the core of a body called an early planetesimal—, a moon-sized type of protoplanet that may have once been much larger, but was perhaps struck many years ago by other heavy orbiting objects, shattering it into pieces, but leaving this particular blob of metal and rock behind. Such collisions were common when the early solar system was forming.

If Psyche was once the heart of a planet with a strong convective current and a molten iron-nickel core at its center, then scientists expect it will still have a magnetic field. A magnetometer aboard the spacecraft will measure its pull, while cameras will photograph and map the surface, collecting high-resolution multispectral images. Because of the asteroid’s unique composition, scientists have no idea what to expect when the images first start rolling in.

“What does an impact crater into metal look like? We do not know?” says Elkins-Tanton.

In a unique twist for this mission, JPL plans to release the images captured by Psyche immediately onto the internet so that anyone can view them within a half-hour of being received.

“We’re not going to edit them or curate them. We’re going to send them out so that everyone can be looking at this funny object for the first time,” says Elkins-Tanton.

In addition, a series of spectrometers will help us understand what the asteroid is made of by measuring the gamma rays and neutrons emitted from it. Depending on what scientists discover, the mission could help answer fundamental questions about the formation of our solar system.

That will depend, of course, on whether the propulsion system functions as designed. As we stand on the precipice of a new era in space exploration, Hall thrusters aren’t just rocket science—they’re the closest thing we have to cosmic alchemy, promising to redefine how we navigate the vast tapestry of our solar system.

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Autumn’s Alchemy: Unveiling the Science Behind California’s High Sierra Fall Foliage

Fall colors changing in the Eastern Sierra (Photo: Erik Olsen)

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Ah, the changing of the leaves—a hallmark of autumn that heralds the end of long summer days and the arrival of crisp, cool weather. The spectacle is especially captivating in the high Sierra region of California, where deciduous trees put on a breathtaking show every year. This year’s show began in early October with an explosion of gold, persimmon, and vibrant orange blanketing the granite crags of the Eastern Sierra.

For years, the Eastern Sierra Fall Color Report has dutifully documented the arrival of Autumn and the magnificent changing hues of millions of trees. But have you ever stopped to wonder why the leaves change color? Why do leaves go from a robust green to vibrant hues of orange, red, and yellow? Well, it’s not just nature’s way of getting all dressed up for Halloween; there’s a complex interplay of biological, chemical, and physical processes at work.

Let’s start with the basics: chlorophyll. During the growing season, leaves are green due to chlorophyll, the molecule that helps plants photosynthesize. Photosynthesis is the process by which plants convert sunlight, water, and carbon dioxide into sugar and oxygen. Chlorophyll’s structure is such that it absorbs blue and red light well but reflects green light, making leaves appear green. However, as the days shorten and temperatures drop, it becomes a signal to the trees that it’s time to get ready for winter.

Structurally, chlorophyll is a complex molecule with a central magnesium ion surrounded by a long hydrocarbon tail. This structure is particularly adept at capturing and utilizing photons from sunlight for photosynthesis. Yet, chlorophyll is also a bit delicate, getting easily damaged by factors like intense light, exposure to oxygen, and even its own activity. That’s why plants are continuously synthesizing it during the growing season. In a sense, chlorophyll is both the engine and the fuel of the plant world, driving the processes that sustain not just the trees themselves but also the ecosystems that rely on them.

Seen through a microscope, chlorophyll is concentrated within organisms in structures called chloroplasts – shown here grouped inside plant cells. By Kristian Peters — Fabelfroh – Self-photographed, CC BY-SA 3.0

As autumn approaches, the biological clock inside trees ticks toward a season of preservation. Photosynthesis slows down, partly because there’s less sunlight but also because the plant is actively throttling this process. As a result, chlorophyll begins to break down and isn’t replenished. Other pigments present in leaves then take center stage, like carotenoids and anthocyanins. Carotenoids are always there, hanging out alongside chlorophyll, but are usually overshadowed by it. They are the ones that give leaves their yellow and orange hues, and are also the molecules that give the pink flamingo its rosy color.

Drone view of changing Fall colors in the Eastern Sierras

Anthocyanins are another class of pigments, but these are a little more high-maintenance; they form only when certain conditions are met. You see, anthocyanins are created through chemical reactions that are influenced by the pH levels in the leaf cells and the amount of sugar that is present. That’s why some years, when conditions are just so—like a warm, sunny fall following a cooler period—you’ll see a dazzling display of red leaves. Anthocyanins absorb light at both the blue and green ends of the spectrum and reflect red light, giving leaves their gorgeous red and purple shades. Anthocyanins are what help give boysenberries their deep purple color.

In California’s high Sierra region, where the elevation provides a unique set of environmental factors, the changing of the leaves can be particularly spectacular. Deciduous trees like the Black Oak, Quaking Aspen, and Dogwood populate these areas. The interplay of sunlight, soil acidity, and temperature variations at higher elevations creates an ideal stage for the full spectrum of fall colors to be displayed. Even within the same species of tree, or sometimes even on the same tree, you can see a diversity of colors due to slight variations in soil composition, moisture, and sunlight exposure.

Changing aspens in the Eastern Sierra (Erik Olsen)

It’s all a spectacular display, but it doesn’t last forever; in fact, the most vibrant colors only last a few weeks. And then the leaves die and fall off. It’s not gravity doing its thing, but rather a biological process called “abscission.” As winter approaches, a layer of specialized cells grows between the leaf stem and the tree, severing the vessels that supply nutrients and water to the leaf. This triggers the leaf to die and eventually fall, making way for new growth in the spring.

While the fall colors in California’s Eastern Sierra are an annual marvel, they’re not immune to the sweeping hand of climate change. Rising temperatures and shifting precipitation patterns have started to tinker with the timing and intensity of the autumnal display. For instance, warmer conditions could delay the onset of the color changes and potentially shorten the duration of peak colors, while altered moisture levels might impact the vibrancy of hues. Even subtle shifts in climate can affect the complex chemistry of leaf coloration. As much as the changing leaves are a symbol of nature’s constancy, they also serve as a barometer for the environmental changes unfolding on a global scale.

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The transformation of leaves in the high Sierra is far more than a seasonal aesthetic; it’s a vivid illustration of how meticulously nature has calibrated life to adapt and thrive. As the leaves cycle through shades of green, orange, red, and finally brown, they tell a tale of survival and renewal, a complex story scripted in their very cells. This fall spectacle is a fleeting moment of brilliance, orchestrated by an array of biological, chemical, and physical processes, each contributing to the grand narrative of life on Earth. In essence, each leaf is a microcosm of resilience and change, characteristics not just of a California autumn, but of life itself.

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The California Gull is the Unsung Hero of Feathered Adaptability and Ecological Balance

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Imagine a bird that’s not only a reliable fixture on both coastal and inland landscapes, but also a winged hero with a knack for saving ecosystems and crops alike. Meet the California gull, a seemingly unassuming creature that’s the avian equivalent of a Toyota Camry: dependable, middle-of-the-road, and surprisingly full of stories. Far from just another seabird scrounging for scraps, this versatile gull is a fascinating study in adaptability, ecological impact, and even historical significance.

Birdwatching might be dismissed as a pedestrian hobby, but when you dive into the details, it’s a riveting blend of science, art, and natural history. Take the task of identifying a gull, for instance. You might think all gulls are created equal, but you’d be sorely mistaken. From the curvature of the bill to the tint of the feathers, each species presents its own unique set of traits. And in this realm, the California gull is the embodiment of middle-of-the-road reliability..

The California gull’s bill is a case study in avian averageness: not too long, not too short, but just right. Then there’s the back—a shade of gray that’s neither too dark nor too light. Size-wise, it’s comfortably nestled between the imposing giants and the pint-sized runts of the gull family. Even its legs are a kind of Goldilocks yellow—nothing too flashy or understated. The same goes for its migration pattern. This bird isn’t setting any long-distance records like the ambitious Arctic terns, nor is it stubbornly clinging to a single geographical point year-round. It moves around a reasonable amount—perhaps 500 to 1,000 miles—but always makes it back to familiar territory in good time.

California gull. (*Larus californicus*) Image: Wikipedia

And where might you spot this paragon of mediocrity? Well, in winter, they’re pretty much where you’d expect any self-respecting gull to be: on beaches, in harbors, hanging around landfills, playgrounds, and fields, or perhaps looking for morsels in tide pools and kelp beds. Come early summer, many venture inland to breed, but they generally make it back to their stomping grounds before the first school bell rings in September.

Yet for a bird that’s so unassuming, the California gull enjoys a surprising level of fame. Case in point: it’s the state bird of Utah, not California. That honor was bestowed upon it for its historical role during the initial Mormon settlement. The Sea Gull Monument in Salt Lake City honors the gull, who saved the people of Utah by consuming the Rocky Mountain crickets which were destroying all the crops in 1848. Quote from monument:

“The Mormon pioneers planted crops in the spring of 1848, after suffering great hunger during their first winter in the Salt Lake Valley. As the crops ripened, hordes of devouring crickets descended upon them from the foothills east of the valley. The Saints fought them with clubs, fire, and water. As they despaired of saving the next winter’s food, their prayers for deliverance from almost sure starvation were answered when thousands of sea gulls came to feed on the crickets. The Sea Gull Monument commemorates this modern-day miracle. The sea gull is now the Utah State bird.”

Sea Gull Monument in Salt Lake City (Wikipedia)

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Moreover, the California gull has been an ecological hero in other ways. At Mono Lake in the Eastern Sierras of California, the gull has had a significant impact on bringing the lake back to life. (The lake is also known for its microbial aliens.) In the early part of the 20th century, Los Angeles’ voracious appetite for water led to shady deals by William Mulholland to secure access to Owens Lake. Declining water levels at Mono Lake threatened the gull population that nested there. But a decisive legal victory by the Save the Mono Lake Committee has ensured the lake is now maintained at healthier water levels, benefiting not just gulls but the entire ecosystem.

However, it’s not all sunny skies for this winged wonder. In the salt pans of South San Francisco Bay, the number of nesting California gulls has exploded—from a mere 24 nests in 1980 to a staggering 45,000 today. It’s a population boom that’s become a double-edged sword. With so many beaks to feed, the California gulls have taken to dining on their neighbors, including baby terns. This poses an ethical conundrum: when is it time to intervene and cull one species to protect another? A tough question—it’s a slippery slope that could eventually loop back to us humans, as we ponder our role in this intricately balanced web of life.

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Through the Looking Glass Head: The Enigmatic World of the Barreleye Fish

The barreleye (*Macropinna microstoma*)
(Courtesy: Monterey Bay Aquarium Research Institute MBARI)

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Off the coast of Monterey, California, researchers captured rare footage of one of the deep sea’s strangest residents: the Barreleye fish. With a see-through head and upward-facing, tube-shaped eyes, it looks like something dreamt up for a sci-fi film. Officially called Macropinna microstoma, this bizarre little fish is a real reminder of how much mystery still lies beneath the surface of the ocean and how otherworldly life can get down there.

First described in 1939, the fish astonished scientists who were stunned by its unique optical anatomy. The barreleye is found in the Pacific Ocean, with sightings ranging from the coasts of California, particularly around Monterey Canyon, to the mid-Pacific near Hawaii. Most commonly, it resides between 400 to 2,500 feet below the surface, a region known as the mesopelagic or “twilight” zone. At these depths, little light penetrates, making the area a seemingly inhospitable place for most life forms. But the Barreleye fish thrives here, adapting to its surroundings in the most bizarre ways.

Its most distinctive features, and the ones that give it its name, are its transparent head and barrel-shaped eyes that are usually directed upwards. These eyes are extremely sensitive to light, which is a scarce commodity where it lives. Interestingly, the eyes are encased in a dome-shaped, transparent head. This clear cranium allows the fish to capture as much light as possible, increasing its visual field. The upward-facing eyes allow the Barreleye fish to see silhouettes of prey or predators against the faint light filtering down from the surface. It’s like a built-in periscope for scanning the world above, allowing it to spot the bioluminescent glow of jellies or small fish that meander above it.

In 2009, researchers at the Monterey Bay Aquarium Research Institute elucidated a longstanding mystery surrounding the barreleye. For many years, marine biologists were under the impression that these specialized eyes were immobile and only provided the fish with a limited, tunnel-vision perspective, focused solely on the waters above its transparent head. Such a constraint would significantly limit the fish’s situational awareness, making it highly dependent on what occurs directly above it for both prey detection and predator evasion.

However, a groundbreaking paper by researchers Bruce Robison and Kim Reisenbichler overturned this conventional wisdom. Their findings reveal that the eyes of the barreleye fish are not static but can actually rotate within a transparent protective shield that envelops the fish’s head. This adaptation enables the fish not only to look upwards to identify potential prey but also to focus forward, thereby expanding its field of vision and facilitating more effective foraging.

A remotely operated vehicle or ROV named Doc Ricketts (MBARI)

Robison and Reisenbichler conducted their research using footage obtained from the Monterey Bay Aquarium Research Institute’s remotely operated vehicles (ROVs) to investigate the barreleye fish in the deep-sea regions adjacent to Central California. Situated at depths ranging from 600 to 800 meters (approximately 2,000 to 2,600 feet) beneath the ocean’s surface, the ROVs’ cameras typically captured images of these fish in a state of immobility, floating like zeppelins with their eyes radiating an intense green hue due to the illumination provided by the ROV’s powerful lighting system. The remotely captured video data also divulged a hitherto undocumented anatomical feature—namely, that the eyes of the barreleye fish are encased in a transparent, fluid-filled protective shield that encompasses the upper region of the fish’s cranial structure.

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The implications of this discovery extend beyond mere academic curiosity. Understanding the unique visual system of the barreleye fish provides crucial insights into the mechanisms of evolutionary adaptation. It showcases how even seemingly minor anatomical modifications can result in significant survival advantages in the highly competitive and challenging marine environment. Moreover, it challenges our existing perceptions and encourages scientists to revisit and reevaluate other long-standing assumptions in marine biology.

The Barreleye isn’t just a pair of eyes swimming around in the ocean, though. It has a suite of other adaptations to its challenging environment. For instance, it has large, flat fins that let it remain almost motionless in the water, conserving energy in an environment where every calorie counts. Also, it’s got a small mouth. This mouth is adapted to consume tiny organisms, like zooplankton, that are abundant in the deep ocean. So while the Barreleye may not be the apex predator down there, it has carved out its own unique niche.

Monterey Bay Aquarium Research Institute (MBARI) in Moss Landing, California

The fish also has what are called “lateral line canals” that are filled with fluid and are sensitive to changes in pressure. This allows the Barreleye to detect movement in the water, effectively giving it a “sixth sense” to sense prey or predators around it. Imagine you’re trying to navigate a pitch-black room—every little bit of extra information helps.

Despite its enigmatic nature, we know relatively little about its breeding habits, lifespan, or social interactions. Part of the reason is the difficulty in studying a creature that lives in such an extreme environment. Researchers have managed to capture only a few specimens, and observations in their natural habitat are relatively scarce.

While the Barreleye fish might look like a figment of a wild imagination, it’s very much a real creature, adeptly adapted to its harsh surroundings. It represents the myriad ways life can evolve to meet the unique challenges of extreme environments. As we continue to explore the depths of our oceans, who knows what other fantastical creatures we might find? That said, the Barreleye fish remains one of the most compelling arguments for the strange and wondrous biodiversity hidden in the ocean’s twilight zone, a testament to the endless creativity of evolution.

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The Ocean’s Invisible Elevator: How Upwelling Fuels California’s Marine Bounty

The Vital Role of Upwelling in California’s Rich Ocean Life

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Few marine processes have been as impactful on the abundance of sea life off the coast of California as upwelling. It may not be a term you’ve heard before, but the natural oceanic process of upwelling is one of the most important engines driving climate, biological diversity, and the ocean’s food web. It’s time to pay attention.

In simple terms, upwelling happens when deep, cold, nutrient-laden water moves toward the ocean surface, replacing the warm surface water. Along the California coast, it’s fueled by the California Current, which flows southward, and by prevailing northerly winds. The wind pushes surface water offshore, allowing the deeper water to well up and take its place. This isn’t just an abstract idea; it’s been studied extensively.

In California, upwelling occurs year-round off the northern and central coast. It’s strongest in the spring and summer when northwesterly winds are at their most powerful. Upwelling is reduced in the fall and winter when winds are more variable.

Killer whales benefit from upwelling because the nutrient-rich waters fuel a surge in phytoplankton, which triggers an increase in the populations of smaller prey fish and marine mammals that orcas rely on for sustenance. (Photo: NOAA)

Researchers from institutions like the Scripps Institution of Oceanography and Stanford University have used a variety of methods, including satellite observations and computer modeling, to study upwelling. One of the groundbreaking studies was the CalCOFI program (California Cooperative Oceanic Fisheries Investigations), which began in the late 1940s. It was a joint venture between Scripps and state and federal agencies to investigate the collapse of the sardine fishery. Over decades, it has expanded its scope and now provides invaluable long-term datasets that help scientists understand the dynamics of upwelling and its effects on marine populations.

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The key to understanding the phenomenon of upwelling off the California coast begins with the importance of cold water. In colder regions, nutrients from the deeper layers of the ocean are more readily brought to the surface through various oceanic processes like upwelling, tidal action, and seasonal mixing.

Think of a well-fertilized garden versus a nutrient-poor one. In the former, you’d expect a lush array of plants that not only thrive, but also support a diversity of insect and animal life. Similarly, the nutrient-rich cold waters support “blooms” of phytoplankton, a critical component of the oceanic food web. Phytoplankton are microscopic, photosynthetic organisms that form the foundation of aquatic food webs, producing oxygen and serving as a primary food source for marine life. When these primary producers flourish, it sets off a chain reaction throughout the ecosystem. Zooplankton (tiny ocean-borne animals like krill) feast on phytoplankton, small fish feast on zooplankton, and larger predators, including larger fish, marine mammals, and seabirds, find an abundant food supply in these teeming waters.

Moreover, cold water has a higher capacity to hold dissolved gases like oxygen compared to warm water (one of the reasons that warming seas could be a problem in the future). Oxygen is a key factor for respiration in marine animals. In cold, oxygen-rich environments, organisms can efficiently carry out metabolic processes, which often results in higher rates of feeding, growth, and reproduction, thereby further boosting biological productivity.

A recent study has also shed light on how California’s rich marine ecosystem responds to climate patterns, particularly the El Niño and La Niña phases of the El Niño/Southern Oscillation (ENSO). Scientists found that during El Niño events, warmer waters and weaker upwelling lead to reduced nutrient levels in the California Current, which supports less phytoplankton and affects the entire food web, including fish populations. In contrast, La Niña conditions boost upwelling, bringing nutrient-rich waters to the surface and enhancing marine productivity. This research highlights the far-reaching impacts of climate cycles on ocean life and could help in forecasting changes that affect fisheries and marine biodiversity in California.

Sardines off the coast of California (Photo: NOAA)

Studies have also shown the direct correlation between the intensity of upwelling and the success of fish populations. A study published in the journal “Science Advances” in 2019 explored how variations in upwelling affect the foraging behavior and success of California sea lions. Researchers found that in years with strong upwelling, sea lions didn’t have to travel as far to find food, which, in turn, positively impacted their population’s health.

Upwelling is a critical oceanic process that helps maintain the stable and immensely productive California marine ecosystem, but there are serious concerns that the dynamics behind upwelling could be changing due to climate change.

Of course, upwelling isn’t just a California thing; it’s a global phenomenon that occurs in various parts of the world, from the coasts of Peru to the Canary Islands. But California is like the poster child, thanks to extensive research and its vital role in a multi-billion dollar fishing industry that includes coveted species like albacore tuna, swordfish, Dungeness crab, squid, and sardines.

Inspiration Point Channel Islands (Photo: NPS)

The Channel Islands provide an excellent example of a place off the California coast where the impacts of upwelling and ocean currents are particularly significant. Channel Islands National Park is uniquely located in a “transition zone” of less than 100 km where many ocean currents converge. This results in strikingly different ocean conditions at individual islands and affects where different species are found and how abundant they are.

Long-term studies of upwelling and the California Current system have shed further light on the importance of these complex and ever changing phenomenon. For example, the annual California Current Ecosystem Status Report captures the big picture of the biology, climate, physical, and social conditions of the marine ecosystem. In 2021, the California Current continued a recent cooling trend, with researchers recording the coldest conditions on the continental shelf in nearly a decade. These cooler coastal waters resulted from strong wind-driven upwelling—nutrient-rich, deep ocean water coming to the surface.

Sea surface temperature anomalies across the northeastern Pacific in August, 2019. A marine heat wave spread across the northeastern Pacific Ocean from 2014 to 2016 and the expanse of warm surface water returned to the region in 2019. (NASA Earth Observatory)

But things have grown more precarious in the north and out to sea. For the last ten years, the northeast Pacific Ocean has been a hotspot for marine heatwaves. Just this past year, scientists monitored the seventh most intense marine heatwave in this region since records began in 1982. However, there was a twist in the tale: unlike in previous years, the elevated water temperatures remained further offshore, a phenomenon partly attributable to stronger-than-average coastal upwelling. As a result, the strip of waters closer to the coast was able to maintain its cooler temperatures, thereby preserving a productive environment for marine life.

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Upwelling is a critical oceanic process that helps maintain the stable and immensely productive California marine ecosystem, but there are serious concerns that the dynamics behind upwelling could be changing due to climate change. Warming ocean temperatures and changes in wind patterns could potentially disrupt the timing and intensity of upwelling, putting the bounty of California’s coast at risk.

Understanding these shifts is imperative for devising strategies to mitigate adverse effects on marine life and commercial fisheries. Therefore, sustained research efforts must continue to dissect this complex (and incredibly important) oceanic process and its increasingly uncertain future.

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Navigating the Unseen Current: How the California Current System Shapes Our Ocean, Climate, and Future

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The stretch of water hugging the western shores of North America is a biological powerhouse, teeming with life and considered one of the most fertile marine environments on the planet. The California Current, originating from the colder regions up near British Columbia, sweeps its way down toward Baja California, extending laterally several hundred miles offshore into deep oceanic waters off the continental shelf. The current brings with it not just frigid waters but also a richness of life. As if choreographed, winds usually gust from the land towards the ocean, nudging surface waters away from the coastline. This displacement makes room for deeper, nutrient-packed waters to ascend, in a phenomenon aptly termed upwelling. Coastal upwelling is the dominant physical forcing affecting production in the California Current System.

This blend of icy waters and nutrient wealth sparks a bloom of marine vegetation, ranging from minuscule phytoplankton to sprawling underwater forests of kelp. These plants, often dubbed the “primary producers,” act as the nucleus of an intricate food web. The bounty includes thriving fisheries, generous populations of marine mammals like whales, seals, and dolphins, as well as a multitude of seabirds. The breadth of this fecund ecosystem can span an astonishing distance—up to 300 miles from the shoreline, enveloping a rich diversity of life within its aquatic embrace.

Phytoplankton are a critical part of the ocean’s food web.

The California Current System (CCS) is one of those natural phenomena that don’t often make headlines but quietly shape life as we know it on the West Coast. It’s like the unsung hero of the Pacific, affecting everything from marine biodiversity to our climate, even having a say in whether you’ll need to pack sunscreen or an umbrella for your beach day.

At its core, the California Current is a cold, southward-flowing oceanic current that starts from the Gulf of Alaska and hugs the western coastline of North America. Picture a river within the ocean, except this river is carrying cold, nutrient-rich water from the North Pacific all the way down to the southern tip of Baja California in Mexico. The California Current is part of a broader gyre system that also includes the North Pacific Current, the California Undercurrent, and the Davidson Current. Together, they create a dynamic dance of currents that provide a lifeline to a host of marine species and play a significant role in weather patterns.

The dynamics of the California Current result in abundant wildlife, like these common dolphins, off the coast of California.

The CCS owes its formation to a combination of factors like Earth’s rotation, the prevailing westerly winds, and the shape of the coastline. These elements work in concert to set up a sort of “conveyor belt” for water, funneling it down from higher latitudes. Over millions of years, this system has become a finely tuned natural mechanism that has shaped the ecology and climate of the region in profound ways.

The cold, nutrient-rich waters of the California Current serve as a veritable buffet for marine life. When we talk about nutrients, we’re primarily talking about nitrates and phosphates that act like fertilizer for phytoplankton, the microscopic plants at the base of the marine food web. As phytoplankton bloom, they become a food source for zooplankton, which in turn are gobbled up by larger fish. This cascade effect supports a rich, biodiverse ecosystem that includes everything from sardines and anchovies to humpback whales and even great white sharks. Even seabirds get in on the action, relying on the abundant marine life for nourishment.

But the California Current doesn’t stop at influencing marine biology; it’s a key player in regional climate as well. For example, the current helps moderate coastal temperatures by funneling cooler air inland. This has a ripple effect on weather patterns and even contributes to the famous “June Gloom” that Angelenos love to lament. Ever wonder why California’s coastal cities have relatively mild, Mediterranean climates while just a short drive inland can bring you much hotter conditions? Tip your hat to the CCS.

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Climate change is, of course, the elephant in the room. A study published in the journal “Geophysical Research Letters” in 2019 highlighted a gradual weakening of the California Current due to warming ocean temperatures. As the current weakens, there’s potential for less upwelling, which means fewer nutrients reaching the surface. Less nutrient-rich water could be a gut punch to the marine food web, affecting fish populations and, by extension, the larger predators and human industries that rely on them.

The cold, nutrient-rich waters of the California Current serve as a veritable buffet for marine life.

Another concern is ocean acidification. The same cold, nutrient-rich waters that make the CCS a hotspot for marine life also make it more susceptible to acidification as they absorb more CO2 from the atmosphere. According to a 2020 study in the journal “Nature,” this could have far-reaching consequences for shell-forming organisms like mollusks and some types of plankton, which play crucial roles in the ecosystem.

So why is all of this important? Well, the California Current is a vital cog in the machinery of our planet. It supports rich biodiversity, influences climate, and even has economic implications, given the commercial fisheries that rely on its abundant marine life. A healthy CCS is good news for everyone, from the weekend beachgoer to scientists concerned about biodiversity.

But as we confront a changing climate, the CCS is a poignant reminder that even the most stable and established natural systems are not immune to disruption. Therefore, understanding it is not just an academic exercise, but a necessary step in safeguarding the fragile balance of life along the western edge of North America.

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The Vital Role of Upwelling in California’s Rich Ocean Life

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