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- Written by: Kara Manke
For nearly half a century, lightning-sparked blazes in Yosemite’s Illilouette Creek Basin have rippled across the landscape — closely monitored, but largely unchecked.
Their flames might explode into plumes of heat that burn whole hillsides at once, or sit smoldering in the underbrush for months.
The result is approximately 60 square miles of forest that look remarkably different from other parts of the Sierra Nevada: Instead of dense, wall-to-wall tree cover — the outcome of more than a century of fire suppression — the landscape is broken up by patches of grassland, shrubland and wet meadows filled with wildflowers more abundant than in other parts of the forest.
These gaps in the canopy are often punctuated by the blackened husks of burned trunks or the fresh green of young pines.
“It really is a glimpse into what the Sierra Nevada was like 200 years ago,” said Scott Stephens, a professor of environmental science, policy and management at the University of California, Berkeley, and co-director of Berkeley Forests.
Stephens is the senior author of a new study that gathers together decades of research documenting how the return of wildfire has shaped the ecology of Yosemite National Park’s Illilouette Creek Basin and Sequoia and Kings Canyon National Parks’ Sugarloaf Creek Basin since the parks adopted policies for the basins — at Illilouette Creek in 1972 and Sugarloaf Creek in 1968 — to allow lightning-ignited fires to burn.
While the prospect of smoke over iconic Half Dome has worried politicians and tourists alike, the work of Stephens and his colleagues demonstrates that allowing frequent fires to burn in these basins has brought undeniable ecological benefits, including boosting plant and pollinator biodiversity, limiting the severity of wildfires and increasing the amount of water available during periods of drought. All these benefits are also likely to make the forest more resilient to the warmer, drier conditions brought by climate change, the research suggests.
“In many ways, fire has successfully been restored to Illilouette, and it has made for a complex mosaic of vegetation with cascading effects on things like water,” said study co-author Brandon Collins, who holds a joint appointment as a research scientist with Berkeley Forests and with the U.S. Forest Service.“In Illilouette, you can have patches of young, regenerating trees from a fire 15 years ago, or areas where a classic understory burn has resulted in big, old, widely-spaced trees. You can even have areas where fire has missed because there’s more moisture, such as adjacent to a creek or on the edge of a meadow. All this complexity can happen in a really short amount of space.”
The study findings arrive in the middle of a critical fire season, when drought conditions throughout the western U.S. have already sparked numerous large wildfires, including the Dixie Fire, which, as of Aug. 8, was the second largest wildfire in California history. While climate change has played a role in increasing the severity of these fires, Stephens said, Illilouette Creek Basin serves as an example of how current forest conditions in the Sierra — largely shaped by decades of fire suppression — are also driving these massive blazes.
“I think climate change is no more than 20 to 25% responsible for our current fire problems in the state, and most of it is due to the way our forests are,” Stephens said. “Illilouette Basin is one of the few places in the state that actually provides that information, because there is no evidence of changes in fire size or in the severity of fires that burn in the area. So, even though the ecosystem is being impacted by climate change, its feedbacks are so profound that it's not changing the fire regime at all.”
Returning fire to Yosemite
For millennia, wildfires sparked by lightning, or lit by Native American tribes, regularly shaped the landscape of the western U.S., not only causing destruction, but also triggering necessary cycles of rebirth and regeneration.
However, the arrival of European colonists in the late 1800s, followed by formation of the U.S. Forest Service in 1905, ushered in an era in which fire was viewed as the enemy of humans and forests alike, and the vast majority of wildfires were quickly extinguished.
By the 1940s and 1950s, a number of forest managers and ecologists had begun to question the wisdom of fire suppression, noting that the practice was eliminating valuable wildlife habitat and increasing the severity of fires by allowing decades of fuel buildup.
These fire proponents included A. Starker Leopold, an acclaimed conservationist and professor of zoology and forestry at UC Berkeley, as well as Harold Biswell, a professor at UC Berkeley’s School of Forestry.
In response to a foundational 1963 report led by Leopold, the U.S. National Park Service changed its policy in 1968 to allow lightning fires to burn within special fire management zones — usually remote regions at high elevations — where danger to human settlements was low. Sequoia and Kings Canyon National Parks established the first fire management zone in 1968, followed by Yosemite National Park in 1972.
“I think it was finally recognized that fire is an integral piece of these ecosystems, and there were a few key people who were willing to take the risk of letting these fires happen,” Collins said.
‘It isn't always clean, and it's not always nice’
Between 1973 and 2016, Illilouette Creek Basin experienced 21 fires larger than 40 hectares — approximately equal to 75 football fields — while Sugarloaf experienced 10 fires of that size. In Illilouette, the result today is a forest that may look a bit messy to the untrained eye, but it holds a lot of resilience.
“When some people visit Illilouette, they say, ‘Look at all these dead trees!’” Stephens said. “I think we have this idea that forests need to be green all the time and made up with only big trees. But it turns out that no forest can do that. It has to be able to grow young trees and regenerate. Illilouette is doing that, but it isn't always clean, and it's not always nice.”
In Illilouette, wildfire has created a more diverse array of habitats for animals like bees and bats, while allowing a variety of plant life to flourish. The detailed history of wildfires in Illilouette has also provided foresters with valuable information on how the impact of one wildfire on landscape and vegetation can influence the trajectory of the next wildfire.
“Since fires are generally allowed to burn freely in Illilouette, we could look at what happens when two fires have burned close to each other: When does the second fire burn into the area that was burned by the first fire, and when does it stop at the previous perimeter?” Collins said. “We found that it really depended on the amount of time that had passed since the first fire. If it had been nine years or under, fires almost never burned into a previous fire perimeter.”
Collins said that Illilouette has also given forest managers a unique opportunity to study how wildfire behaves under a variety of conditions, rather than only at its most dire.
“One of the things that's kind of perverse about the fire suppression policy is that we actually constrain fires to only burn under the worst conditions. If the fire is mellow, that's a good time to put it out, and, as a result, they only burn when we can't put them out,” Collins said. “But by letting these fires burn [in Illilouette], they're able to experience the full range of weather conditions. On bad days, some of these fires have really put up a pretty good plume. But on the flip side, they also get to burn under more moderate conditions, too, and it makes for really varied effects.”
Returning fire to Illilouette has also had the somewhat counterintuitive impact of increasing the availability of water in the basin, a key finding as California weathers yet another year of extreme drought.
Study co-author Gabrielle Boisramé, an assistant research professor at the Desert Research Institute in Nevada, began studying water in Illilouette as a Ph.D. student in environmental engineering at UC Berkeley. Her simulations and measurements indicate that small gaps in the tree canopy created by wildfires have allowed more water from snow and rainfall to reach the ground, while also reducing the number of trees competing for water resources. As a result, soil moisture in some locations in Illilouette increased as much as 30% between 1969 and 2012, which likely contributed to very low tree mortality in the basin during the drought years of 2014 and 2015.
Measurements also indicate that streamflow out of Illilouette Creek Basin has increased slightly since the managed wildfire program began, while streamflow out of other similar watersheds in the Sierras have all decreased. Boosting the amount of water that flows downstream is likely to benefit both the humans and the aquatic ecosystems that depend on this precious resource.
“There's more and more work being done that examines the effects of fire on hydrology, but most of the other research is looking at the effects of catastrophic fires that burned up an entire forest,” Boisramé said. “As far as we know, we're the only ones in the western U.S. studying a restored fire regime, where we’re not just looking at one individual fire, but a number of fires of mixed severity that have occurred over natural intervals of time. There just aren’t that many places to study the long-term effects of these repeated wildfires because Sugarloaf and Illilouette were the first areas in California — really the first western mountain watersheds — where they started allowing fires to burn most of the time.”
Fighting for fire
Most U.S. national parks now practice some form of fire use, rather than full fire suppression, and in 1974, the National Forest Service also changed its policy to also allow some fires to burn on its lands, although areas of fire use are rare in this agency. However, these federal fire use policies have struggled to gain a foothold, largely because of the inherent risks involved in managing wildfire.
Even in Sugarloaf Creek Basin, where many fires have been allowed to burn, there has also been significantly more fire suppression than in Illilouette, the study found. As a result, the ecological benefits in Sugarloaf are not as pronounced as those in Illilouette.
“I think one of the key things to recognize is that the landscape in Illilouette was already somewhat unique, partly because it is at slightly higher elevation than a lot of the forests we manage,” Collins said. “As a result, it already had a mix of vegetation with patches of meadows and rock, and I think maybe that gave managers a little more ease in letting fire happen there. It doesn't have the potential to really push off a giant megafire because it lacks the continuity that some of these other areas have.”
While both naturally-sparked fires and prescribed burns could help large swathes of the Sierra forest become more resilient to both drought and high severity fire, opposition to national “let it burn” policies in California remains strong, with state and local fire agencies often favoring the safety of fire suppression.
Collins and Stephens both acknowledge that the current fuel density in much of the Sierra, mixed with the hotter, drier conditions already triggered by climate change, has made managing wildfire even riskier than it was when forest managers started allowing fires to burn in Yosemite in 1972. However, they argue, fire suppression will never succeed in the long term, because the longer that forest fuel sources are allowed to build up, the more likely it becomes that wildfires will turn catastrophic when they are finally sparked.
“In order to actually allow this to happen, political and public institutions need to be willing to accommodate risk, because there will be some unpredictability. There are going to be fires that get larger, and more severe burning in places that have had very little fire for a century or more,” Stephens said. “We can't guarantee that Illilouette is going to be the new outcome, because it started when climate change was not nearly as severe. So, political institutions will have to accommodate that, or the first fire that doesn't do exactly what we hope will shut down the whole program.”
Collins and Stephens also advocate for more aggressive prescribed burning and restoration thinning throughout the Sierra to help get the forests to a place where lightning-sparked fires can be allowed to burn more safely.
Stephens credits strong, early leadership at Yosemite — including that of study co-author Jan W. van Wagtendok, who received a Ph.D. from UC Berkeley in 1972 and went on to serve as a research scientist at Yosemite for most of his career — for taking the huge risk of launching the program and allowing early fires to burn in the park.
“It's been 50 years now, but I think what we've learned helps us understand what is possible,” Stephens said. “We have 10 to 20 years to actually change the trajectory of the forest ecosystems in our state, and if we don't change them in 10 or 20 years, the forest ecosystems are going to change right in front of our eyes, and we're just going to be passengers. That's why it's so important to continue this work.”
Previous funding from the U.S. Joint Fire Science Program, UC ANR Competitive Grants Program, and the National Science Foundation’s Critical Zone Collaborate Network (award number 2011346) supported the research in this paper.
Study co-authors also include Sally Thompson of the University of Western Australia; Lauren C. Ponisio of the University of Oregon, Eugene; Ekaterina Rakhmatulina, Jens Stevens and Zachary L. Steel of UC Berkeley; and Kate Wilkin of San Jose State University.
Kara Manke writes for the UC Berkeley News Center.
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- Written by: Elizabeth Larson
Dogs available for adoption this week include mixes of husky, Labrador retriever, pit bull, Rhodesian Ridgeback, Rottweiler and shepherd.
Dogs that are adopted from Lake County Animal Care and Control are either neutered or spayed, microchipped and, if old enough, given a rabies shot and county license before being released to their new owner. License fees do not apply to residents of the cities of Lakeport or Clearlake.
The following dogs at the Lake County Animal Care and Control shelter have been cleared for adoption (additional dogs on the animal control website not listed are still “on hold”).
Call Lake County Animal Care and Control at 707-263-0278 or visit the shelter online at http://www.co.lake.ca.us/Government/Directory/Animal_Care_And_Control.htm for information on visiting or adopting.
Female pit bull puppy
This female pit bull puppy has a tan and white coat.
She is in kennel No. 4a, ID No. LCAC-A-1324.
Female pit bull puppy
This female pit bull puppy has a white coat.
She is in kennel No. 4b, ID No. LCAC-A-1325.
Female pit bull puppy
This female pit bull puppy has a tan coat.
She is in kennel No. 4c, ID No. LCAC-A-1328.
Male pit bull puppy
This male pit bull puppy has a tan and white coat, and blue eyes.
He is in kennel No. 5a, ID No. LCAC-A-1323.
Male pit bull puppy
This male pit bull puppy has a tan coat and blue eyes.
He is in kennel No. 5b, ID No. LCAC-A-1326.
Male pit bull puppy
This male pit bull puppy has a brown and white coat, and blue eyes.
He is in kennel No. 5c, ID No. LCAC-A-1327.
Male Labrador retriever
This 2-year-old male Labrador retriever has a short black coat with white markings.
He is in kennel No. 19, ID No. LCAC-A-1349.
‘Dusty’
“Dusty” is a 2-year-old female pit bull terrier mix with a short gray coat.
She is in kennel No. 22, ID No. LCAC-A-611.
‘Jim’
“Jim” is a 2-year-old pit bull terrier mix with a short black and white coat.
He is in kennel No. 23, ID No. LCAC-A-810.
‘Rosco’
“Rosco” is 3-year-old a male Rhodesian Ridgeback-Shepherd mix with a short tan coat.
He is in kennel No. 25, ID No. LCAC-A-1205.
Rottweiler-pit bull mix
This 1-year-old female Rottweiler-pit bull mix has a short black coat.
She has been spayed.
She is in kennel No. 27, ID No. LCAC-A-731.
Female pit bull terrier
This 4-year-old female pit bull terrier mix has a short white coat.
She is in kennel No. 29, ID No. LCAC-A-812.
‘Bubba’
“Bubba” is a male pit bull terrier mix with a short black coat.
He is in kennel No. 30, ID No. LCAC-A-1306.
Male husky
This 2-year-old male husky has a red and cream coat.
He is in kennel No. 32, ID No. LCAC-A-1024.
‘Ghost’
“Ghost” is a 2-year-old female husky with an all-white coat and blue eyes.
She is in kennel No. 34, ID No. LCAC-A-1167.
Email Elizabeth Larson at
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- Written by: John Tarduno, University of Rochester
Surrounding Earth is a powerful magnetic field created by swirling liquid iron in the planet’s core. Earth’s magnetic field may be nearly as old as the Earth itself – and stands in stark contrast to the Moon, which completely lacks a magnetic field today.
But did the Moon’s core generate a magnetic field in the past?
In the 1980s, geophysicists studying rocks brought back by Apollo astronauts concluded the Moon once had a magnetic field that was as strong as Earth’s. But a robust magnetic field requires a power source, and the Moon’s core is relatively small. For decades, scientists have struggled to resolve this conundrum: how could such a small core create a strong magnetic field?
I’m a professor of geophysics and have been studying Earth’s magnetic field for more than 30 years. I recently assembled a team to use new scientific techniques to reexamine the evidence for lunar magnetization. We found that the Moon did not in fact have a long-lived magnetic field. Not only does this finding change the modern understanding of the Moon’s geologic history, it also has major implications for the presence of resources on the Moon that could be critical to future human exploration.
Why a magnetic Moon?
Certain rocks have the extraordinary ability to preserve records of past magnetic fields when they contain minerals with iron atoms that align with a magnetic field as the rock cools and solidifies. The best magnetic minerals at preserving evidence of a field are tiny – a thousand times smaller than the width of a human hair – because it takes a lot of energy to rearrange their atoms.
Geophysicists who study ancient magnetism recreate this process, reheating rock samples in the presence of known magnetic fields and comparing the new alignment of the iron atoms with the orientation of iron atoms before the rock was reheated. This allows researchers to learn about past magnetic fields.
Early researchers studying the first rocks brought back from the Moon by U.S. astronauts wanted to use this method to study the Moon’s magnetism. But they faced problems. Lunar rocks contain a certain type of iron – called native iron – that is easily altered by heat. Additionally, the native iron grains in lunar rocks are sometimes relatively large, making them less likely to reliably record past magnetic fields.
From the 1970s onward, geophysicists used alternative, nonheating methods to study the Moon’s magnetism. They found that some lunar samples had recorded strong magnetic fields, suggesting that the Moon had a magnetic field for over 2 billion years.
But this result only deepened the conundrum. The question of how the Moon’s core could produce a strong magnetic field remained unsolved.
An alternative theory
In the experiments, some Apollo samples showed evidence of strong magnetic fields but other samples did not. Some researchers attributed the missing magnetization to the presence of large native iron grains that were poor magnetic recorders. But many of the samples also contained small iron grains that should have recorded a field.
There have been long-standing doubts about the nonheating techniques researchers used on the Apollo samples. Some scientists have called them methods of “last resort” and conclude that the uncertainties in data collected in this way were so large that any interpretation must be viewed as speculation.
Alternatively, another group of scientists has suggested for decades that when meteorites strike the Moon, they create a dusty plasma – a gas of ions and electrons – that could generate a strong magnetic field and magnetize lunar rocks near the impact zone.
In 2008, geophysicist Kristin Lawrence decided to revisit the question of lunar magnetization using an improved reheating technique. In contrast to the researchers who originally studied the samples, she was unable to detect any definitive evidence for a past magnetic field. The approach Lawrence and her team used was better than the nonheating tests, but her results were still not conclusive. She felt she was on to something, though, and that is when she turned to me and my lab for help.
In 2011, Lawrence brought us a collection of lunar samples to test. We had been developing techniques to identify individual millimeter-size silicate crystals that contain only very small iron grains and have ideal recording properties. We then used an ultrasensitive superconducting magnetometer and a special carbon dioxide laser to rapidly heat those samples in a way that avoids altering their iron minerals. We found that nearly all the rocks had profoundly weak magnetic signals.
At the time of this first test we were still improving the method, so we couldn’t say with certainty whether the samples had formed on a Moon without a magnetic field. But we have been improving our testing methods, and last year we decided to revisit the Apollo samples.
We definitively found that some of the samples did indeed contain magnetic minerals capable of preserving high-fidelity signals of ancient magnetic fields. But the rocks had recorded no such signals. This suggests that the Moon lacked a magnetic field for nearly all of its history.
So, what explains the previous findings of a magnetic Moon? The answer was in one of the samples: a small, dark piece of glass containing tiny iron-nickel particles.
The glass was made by a meteorite impact and showed clear evidence of a strong magnetic field. But it was formed only about 2 million years ago. Nearly all geophysicists agree the Moon did not have a magnetic field at that time, because after 4.5 billion years of cooling there was not enough heat left to power the churning of iron in the Moon’s core to generate a field. The magnetic signature of the glass matched simulations of magnetic fields that can be generated by meteor impacts. This showed that meteorite impacts alone can create strong magnetic fields that magnetize rocks nearby. This could explain the high values previously reported from some Apollo rocks.
Taken together, I believe these findings resolve the mystery of a seemingly magnetic Moon.
Magnetic shielding and lunar resources
This new view of lunar magnetism has huge implications for the potential presence of valuable resources as well as information about the ancient Sun and Earth that may be buried in lunar soils.
Magnetic fields act as shields that prevent solar particles from reaching a planet or moon. Without a magnetic field, solar wind can hit the surface of the Moon directly and implant elements like helium-3 and hydrogen into the soil.
Helium-3 has many applications, but importantly, it could be a fuel source for nuclear fusion and future planetary exploration. The value of hydrogen comes from the fact that it can combine with oxygen to form water, another crucial resource in space.
Since the Moon did not have a long-lived magnetic field, these elements could have been accumulating in soils for billions of years longer than previously thought.
There is also scientific value. Elements embedded by solar wind could shed light on the evolution of the Sun. And as the Moon passes through Earth’s magnetic field, elements from Earth’s atmosphere can be deposited on the lunar surface, and these may hold clues about the earliest Earth.
The absence of a long-lived magnetic field on the Moon might strike some as a loss, but I believe it may unlock a scientific bonanza and a valuable stash of potential resources.
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John Tarduno, Professor of Geophysics, University of Rochester
This article is republished from The Conversation under a Creative Commons license. Read the original article.
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- Written by: Elizabeth Larson
LAKE COUNTY, Calif. — The National Weather Service has issued a weekend heat advisory for Lake County, while the Lake County Air Quality Management District is warning of continued smoky air conditions due to large wildland fires around the region and Oregon.
The weather advisory is in effect from 1 p.m. Saturday to 8 p.m. Sunday.
The local forecast calls for daytime highs of between 104 and 108 on Saturday and Sunday, with higher temperatures expected in Middletown.
Nighttime temperatures are forecast to be in the low 60s, with light winds of around 10 miles per hour in the afternoons and evenings.
On Monday, temperatures are expected to be around the century mark before rolling back into the 90s through Friday.
At the same time, the National Weather Service forecast says those hot temperatures will be paired with widespread haze through the start of the week.
The Lake County Air Quality Management District said the source of the smoke and haze continues to be the Dixie, McFarland, Monument the River Complex fires, as well as other fires burning in Northern California and Oregon.
The district said overall air quality late this week has remained “moderate” to “unhealthy for sensitive groups.”
The air quality forecast for the weekend will range from “moderate” to “unhealthy for sensitive groups.” There is a moderate potential for “unhealthy for all” conditions when strong inversion conditions develop in the overnight hours, the district reported.
The regional weather patterns are expected to keep the heaviest smoke concentrations north of the air basin, according to the district report.
While the smoke event continues, area residents are encouraged to minimize outdoor activities, especially exercise, not to use fans that bring smoky air inside, run air conditioners on the “recirculate” or “recycle” setting and change standard air filters to medium or high efficiency filters.
Links for air quality conditions and air monitoring are available at the Lake County Air Quality Management District website.
Email Elizabeth Larson at
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