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    COP28 is making headlines. Here’s why the focus on methane matters

    This year’s United Nations’ annual climate summit, dubbed COP28, is making a lot of headlines — not something I would have found myself writing a few years ago.

    One reason for COP’s higher profile is a growing sense of urgency to take stronger action to reduce humans’ fossil fuel emissions and mitigate the looming climate crisis. The world is nowhere near on track to meet the goals of the 2015 Paris Agreement — that is, reducing greenhouse gas emissions sufficiently to limit global warming to “well below” 2 degrees Celsius of preindustrial averages by the year 2100 (SN: 12/12/15). Meanwhile, 2023 has been the hottest year on record, people have been suffering through a barrage of extreme weather events, including heat waves, droughts and floods, and 2024 is likely to break more temperature records (SN: 12/6/23; SN: 7/19/23).

    The headlines emerging from COP28 have been a mix of pleasing, frustrating and bewildering. For example: It’s good news that 198 nations have ratified the Loss and Damage Fund, a formal acknowledgment by wealthy, high-polluting nations that they should help mitigate the rising costs of climate change faced by developing nations. But it’s frustrating that the pledges by the wealthy nations so far amount to just about $725 million, less than 0.2 percent of the annual climate change–linked losses faced by developing nations.

    For me, one of the biggest questions related to those headlines pertains to methane. It feels unclear whether, on balance, there’s more good or bad news when it comes to emissions of that second most important human-caused greenhouse gas.

    Methane is a powerhouse climate-warming gas, with about 80 times the atmosphere-warming potential of carbon dioxide. However, methane has a saving grace: It mercifully lingers for only about a decade in the atmosphere (SN: 4/22/20). Carbon dioxide can stick around for up to 1,000 years. Cutting methane emissions can mean its atmospheric concentration drops relatively rapidly.

    The Global Methane Pledge, launched two years ago at COP26, may be gaining some momentum, but it still lacks the sign-on of key big-emitting nations. Then there’s the December 1 announcement by 49 oil and gas companies that they would reduce methane leaks from their infrastructure to “near zero” by 2030, which seems like a good thing on the face of it but has also been called greenwashing (SN: 11/24/21).

    And all of this policy wrangling is happening against a bizarre backdrop: a startling, puzzling, worrisome sharp increase in methane emissions over the last decade — not from humans, but from natural sources, particularly wetlands.

    To help me sift through the headlines and better understand all the news that’s seeping out, I talked with Euan Nisbet, a geochemist at Royal Holloway, University of London in Egham.

    Methane “is rising very fast,” Nisbet says. “So fast it looks like the Paris Agreement is going to fail.”

    Countries are promising to cut methane emissions

    While the rise in natural methane emissions is worrisome, about 60 percent of current methane emissions into the atmosphere still comes from human activities. Methane doesn’t just seep out of leaky oil and gas pipelines or get pumped into the air during coal combustion. Agriculture, including ruminant animals, are a big source (SN: 5/5/22). Landfills are another (SN: 11/14/19).

    That’s where the Global Methane Pledge comes in, promising a 30 percent cut in humans’ emissions by 2030. The pledge was spearheaded in 2021 by the United States and the European Union, and so far, 150 nations have signed on. Most recently, Turkmenistan, which has sizable methane emissions, joined. So there’s hope: If everyone were to follow suit, it really is possible to cut global methane emissions deeply, bringing us much closer to meeting the Paris Agreement’s goals, Nisbet argues in a Dec. 8 editorial in Science.

    Still, many of the world’s biggest methane emitters, including China, India, Russia, Iran and South Africa, have not signed on to the pledge. China’s methane comes in large part from its coal combustion; India’s, from coal as well as waste heaps and biomass fires. And China alone currently releases an estimated 65 million metric tons of methane per year, more than double that of the United States or India, the next two biggest emitters.

    With only seven years left before the 2030 deadline, meeting the global pledge’s methane reduction goals would be steep — but, Nisbet says, not impossible.

    There’s precedent for successfully making such steep cuts to methane in such a short time, he adds. During the 2000s, “there was a seven-year period where [the U.K. government] brought methane emissions down by 30 percent,” in large part by reducing emissions from landfills and gas leaks.

    China has just released its own Methane Emissions Control Action Plan in November, alongside a joint commitment between China and the United States to take action on methane. That news sounds potentially promising, if not wholly reassuring, as the plan does not include a lot of concrete numbers, Nisbet says.

    So, what about the oil and gas industry’s recent promise to address its leaky infrastructure? Such a promise also sounds positive on the face of it — leaky infrastructure is definitely the low-hanging fruit when it comes to reducing humans’ methane emissions to the atmosphere (SN: 2/3/22).

    On the other hand, hundreds of scientific and environmental organizations have signed an open letter in response. The letter suggests that the oil and gas industry’ promise is just greenwashing, “a smokescreen to hide the reality that we need to phase out oil, gas and coal,” the letter states. Furthermore, many oil and gas companies may routinely abandon old, still-leaking wells — effectively eliminating those leaks from their company’s emissions roster without actually stopping them.

    That said, addressing the leaks does have to be done, Nisbet says. “I’d love to shut down the coal industry quickly, but I’m aware of the enormous social problems that brings. It’s a very difficult thing to nuance. You can’t go cold turkey. We’ve got to wind it down in an intelligent and collaborative way. The best thing to do is to stop the crazy leaks and venting.”

    Natural methane emission has been surging

    Plugging the leaks as soon as possible has taken on an increasing urgency, Nisbet says, because of a stark rise in natural methane being emitted to the atmosphere. Why this rise is happening isn’t clear, but it seems to be some sort of climate change–related feedback, perhaps linked to changes in both temperature and precipitation.

    That natural methane emissions bump was also not something that the architects of the Paris Agreement saw coming. Most of that rise has happened since the agreement was signed. From 1999 to 2006, atmospheric methane had spent several years in near-equilibrium — elevated due to human activities, but relatively stable. Then, in 2007, atmospheric methane concentrations began to increase. In 2013, there was a particularly sharp rise, and then again in 2020.

    Much of that increase seems to have come from tropical wetlands. Over the past decade, researchers have tracked shifts in methane sources by measuring carbon-12 and carbon-13 in the gas. The ratio of those two forms of carbon in the methane varies significantly depending on the source of the gas. Fossil fuel-derived methane tends to have higher concentrations of carbon-13 relative to carbon-12; methane from wetlands or agriculture tends to be more enriched in carbon-12.

    The recent spikes in natural methane are eerily reminiscent of ice core records of “glacial termination” events, times in Earth’s deep past when the world abruptly shifted from a glacial period to a period of rapid warming, Nisbet and others reported in June in Global Biogeochemical Cycles. Such glacial termination events are large-scale reorganizations of the ocean-atmosphere system, involving dramatic changes to the circulation of the global ocean, as well as to large climate patterns like the Indian Ocean Dipole (SN: 1/9/20).

    “Is this comparable to the start of a termination event? It looks horribly like that,” Nisbet says. But “it may not be. It might be totally innocent.”

    Right now, scientists are racing to understand what’s happening with the natural methane bump, and how exactly the increased emissions might be linked to climate change. But as we search for those answers, there is something that humans can and must do in the meantime, he says: Cut human emissions of the gas as much as possible, as fast as possible. “It’s very simple. When you’re in a hole, stop digging.” More

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    Landscape Explorer shows how much the American West has changed

    With the click of a mouse, a new mapping tool shows how places in the American West have changed over the last 70 years.

    With just a Web browser, anyone can open Landscape Explorer, which will pull up a modern Google map of the United States beside a black-and-white aerial image of the western states circa 1950. A slider button allows for scrolling back and forth between past and present.

    You can type a place or address into the search bar, then zoom in or out. Search for “Lake Powell” and watch the Colorado River’s red rock canyons of the past turn into a reservoir. Type in “Las Vegas” and see Sin City’s sprawling grid of streets disappear into desert arroyos as you swipe back in time.

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    The free tool is an easy way for anyone with an interest in the American West to peruse the past. But Landscape Explorer also has a loftier purpose: helping government agencies, landowners and conservation professionals make complex decisions about how to manage land.

    The powerful visual contrast between the historical snapshot and modern-day satellite imagery “allows us to go from zero to 100” in terms of understanding ecosystem changes, says Scott Morford, an applied spatial ecologist at the University of Montana in Missoula who led the development of Landscape Explorer. The project was supported by Working Lands for Wildlife, a conservation initiative led by the U.S. Department of Agriculture, and other partners. The impetus, Morford says, was to “give us a reference for how rapidly things are changing across biomes that we care about.”

    Before Landscape Explorer, most collections of historical imagery of large-scale landscapes went back to only the 1980s. Finding earlier imagery of large landscapes was expensive and time-consuming. While some previous projects have stitched together historical imagery at small scales to look at how a particular watershed or county has changed, “the real revolution is that we were able to figure out how to do it at scale,” Morford says. “We wanted to make something that was universal and accessible” for everyone, not just remote sensing specialists.

    Morford and colleagues processed about 170,000 aerial images that were taken by U.S. Army pilots during the Cold War and later digitized. To create a continuous mosaic, the team used specialized software to stitch together images of adjacent patches of land, the researchers explained in a paper published in July in Remote Sensing in Ecology and Conservation. The final step was pairing the mosaic with satellite imagery using Google Earth Engine.

    Landscape Explorer began as a small project to assess the extent of woody encroachment onto grasslands in western Montana. Due to fire suppression, conifers like western juniper or eastern red cedar are taking over ecosystems that were historically treeless, such as sagebrush steppe and prairies. A monoculture of these water-guzzling trees is bad news for local biodiversity and increases the risk of catastrophic wildfire.

    Third-generation Montana rancher Bruce Peterson says that seeing historical and current aerial imagery side by side made him realize how the steady infiltration of trees had devalued his family’s livestock pastures. “It’s a little bit like losing your hearing or your vision with these trees. They eat away a little of your land at a time, and then by the time you get hearing aids or glasses, you realize it’s gotten really out of hand,” Peterson says.

    Using Landscape Explorer, Peterson and dozens of other landowners involved in the Southwest Montana Sagebrush Partnership have prioritized where to remove invading trees. The group has restored nearly 50,000 acres of treeless rangeland since 2020, according to the Nature Conservancy, a member of the partnership.

    Landscape Explorer also helped the Clark Fork Coalition, a Montana-based nonprofit that protects and restores waterways, to see how urban and industrial development has impacted floodplains. “This tool gives us the power of time travel. It’s like a time-lapse showing all that’s been lost and where the continued pressure is very real,” says Karen Knudsen, the coalition’s executive director.

    After seeing the successes in Montana, the makers of Landscape Explorer extended the tool to 17 states in the West to show where forests, grasslands or rivers are most at risk of disappearing and where intact habitats can still be preserved.

    Since the expanded tool was released in September, researchers have used it to assess glacial retreat in the Pacific Northwest, measure the historical extent of sand dunes in coastal California and pinpoint where wetlands have dried up. Morford is excited to see all the ways Landscape Explorer can help land managers. “It’s going to be used in ways we haven’t even thought of yet.” More

  • in

    A new UN report lays out an ethical framework for climate engineering

    The world is in a climate crisis — and in the waning days of what’s likely to be the world’s hottest year on record, a new United Nations report is weighing the ethics of using technological interventions to try to rein in rising global temperatures.

    “The current speed at which the effects of global warming are increasingly being manifested is giving new life to the discussion on the kinds of climate action best suited to tackle the catastrophic consequences of environmental changes,” the report states.

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    A broad variety of climate engineering interventions are already in development, from strategies that could directly remove carbon dioxide from the atmosphere to efforts to modify incoming radiation from the sun (SN: 10/6/19; SN: 7/9/21; SN: 8/8/18).

    But “we don’t know the unintended consequences” of many of these technologies, said UNESCO Assistant Director-General Gabriela Ramos at a news conference on November 20 ahead of the report’s release. “There are several areas of great concern. These are very interesting and promising technological developments, but we need an ethical framework to decide how and when to use them.”

    Such a framework should be globally agreed upon, Ramos said — and that’s why UNESCO decided to step in. The new report proposes ethical frameworks for both the study and the later deployment of climate engineering strategies.

    In addition to explicitly addressing concerns over how tinkering with the climate might affect global food security and the environment, ethical considerations must also include accounting for conflicting interests between regions and countries, the report states. Furthermore, it must include assessing at what point the risks of taking action are or are not morally defensible.   

    “It’s not [for] a single country to decide,” Ramos said. “Even those countries that have nothing to do with those technological developments need to be at the table … to agree on a path going forward. Climate is global and needs to be a global conversation.”

    The ethics-focused report was prepared by a UNESCO advisory body known as the World Commission on the Ethics of Scientific Knowledge and Technology. Its release coincided with the start of the U.N.’s international climate action summit, the 28th Conference of the Parties, or COP, in Dubai. COP28 runs from November 30 through December 12.

    To delve more into the goals of the study and what climate engineering strategies the report considers, Science News talked with report coauthor Inés Camilloni, a climate scientist at the University of Buenos Aires and a resident in the solar geoengineering research program at Harvard University. The conversation has been edited for length and clarity.

    SN: There have been a lot of reports recently about climate engineering. What makes this one important?

    Camilloni: One thing is that this report includes the views from the Global South as well as the Global North. This is something really important, there are not many reports with the voices of scientists from the Global South. The U.N. Environment Programme’s report this year [on solar radiation modification] was another one. [This new report] has a bigger picture, because it also includes carbon dioxide removal.

    I’m a climate scientist; ethics is something new to me. I got involved because I was a lead author of a chapter in the [Intergovernmental Panel on Climate Change] 1.5-degrees-Celsius special report in 2018, and there was a box discussion about climate engineering (SN: 10/7/18). I realized I was not an expert on that. The discussion was among scientists in the Global North, who had a clear position in some ways about the idea, but not Global South scientists. We were just witnessing this discussion.

    SN: The report raises a concern about the “moral hazard” of relying too much on climate engineering, which might give countries or companies an excuse to slow carbon emission reductions. Should we even be considering climate engineering in that context?

    Camilloni: What we are saying in the report is that the priority must be the mitigation of greenhouse gas emissions. But the discussion on climate engineering is growing because we are not on track to keep temperatures [below] 1.5 degrees C. We are not [at] the right level of ambition really needed to keep temperatures below that target. There are so many uncertainties that it’s relevant to consider the ethical dimensions in these conversations, to make a decision of potential deployment. And in most IPCC scenarios that can limit warming to below 1.5 degrees, carbon dioxide removal is already there.

    SN: What are some of the carbon dioxide removal strategies under consideration?

    Camilloni: Carbon dioxide removal combines two different methods: Restoring natural carbon sinks, like forests and soils, and investing in technologies that are maybe not yet proven to work at the scale that’s needed. That includes direct air capture [of carbon dioxide] and storage; bioenergy with carbon capture and storage; increasing uptake by the oceans of carbon dioxide, for example by iron fertilization; and enhancing natural weathering processes that remove carbon dioxide from the atmosphere.

    But there are potential consequences that need to be considered. Those include negative impacts of terrestrial biodiversity, and effects on marine biodiversity from ocean fertilization. As for sequestering carbon dioxide — how do you store it for hundreds of years or longer, and what are the consequences of rapid release from underground reservoirs? Also there’s potential competition for land [between bioenergy crops or planting trees] and food production, especially in the Global South.

    SN: Solar radiation modification is considered even more controversial, but some scientists are saying it should now be on the table (SN: 5/21/10). What type of solar radiation modification is the most viable, technologically?

    Camilloni: That’s an umbrella term for a variety of approaches that reduce the amount of incoming sunlight reflected by the atmosphere back to space.

    There’s increasing surface reflectivity, for example with reflective paints on structures, or planting more reflective crops (SN: 9/28/18). That reflects more solar radiation into space. It’s already being used in some cities, but it has a very local effect. Similarly, increasing the reflectivity of marine clouds — there were some experiments in Australia to try to protect the Great Barrier Reef, but it seems that also the scale is not global.

    Another proposed strategy is to thin infrared-absorbing cirrus clouds — I don’t really know much about that or if it’s really possible. And there’s placing reflectors or shields in space to deflect incoming solar radiation; I also don’t really know if it’s possible to do that.

    Injecting aerosols into the stratosphere, to mimic the cooling effect of a volcanic eruption, is the most promising for a global impact. It’s not so challenging in terms of the technology. It’s the only way that we have identified that can cool the planet in a few years.

    SN: How soon could aerosol injection be used?

    Camilloni: We need at least 10 to 20 years before we can think of deployment. The limitation is that we need the aircraft that can fly at around 20 kilometers altitude. Those are already being designed, but we need about 10 years for those designs, and another 10 to build a fleet of them.

    SN: What are some of the ethical concerns around aerosol injection or other solar radiation modification technologies?

    Camilloni: These new technologies may be risky in the potential for exacerbating climate problems or introducing new challenges. There are potential risks to changing precipitation patterns, even overcooling in some regions. A key consideration in deciding whether to pursue them is the need for a full characterization of the positive and negative effects of the different technologies around the globe, and a comparison against the risk of not intervening.

    SN: In 2021, a research group at Harvard was barred from launching a balloon into the stratosphere to test equipment for possible future aerosol release. How might this report address similar studies?

    Camilloni: In our report, we want to make a distinction among the different types of research. You can have indoor research — simulations, social analysis — and this is not so controversial. When you consider outdoor research — releasing particles into the atmosphere — that is more controversial. We are calling for more indoor research. We need to understand the potential impacts.

    [For example,] I studied the impact of solar radiation modification on the hydrology of the La Plata Basin [which includes parts of southeastern Brazil, Bolivia, Paraguay, Uruguay and northeastern Argentina]. It’s the most populated region on the continent, and very relevant for hydropower production. And it’s already a very impacted region by climate change.

    However, that research was based on just one climate model. We need more — more resources, more capacity building in the Global South. My research group was the first to explore those impacts in Latin and South America. There are others doing research on this over the next few months, but I can count those groups on one hand.

    We need more resources to be part of any discussion. Those resources include the Loss and Damage Fund to provide support to nations most vulnerable to the climate crisis [agreed to at the end of COP27 in 2022]. But nobody really knows now how that will be implemented.

    SN: The report’s release was timed to the start of COP28. What are you hoping that policymakers will take away from it over the next two weeks?

    Camilloni: These recommendations are really important to have in mind, of course. We need more research to make a decision about whether this is a good idea or a bad idea. And maybe people will cut admissions faster if they’re afraid of climate engineering. More

  • in

    This bird hasn’t been seen in 38 years. Its song may help track it down

    How do you look for an animal you don’t even know exists anymore?

    The last sighting of the purple-winged ground dove (Paraclaravis geoffroyi) — a small, bamboo-loving dove native to the South American Atlantic Forest in Brazil, Argentina and Paraguay — was in 1985. But, researchers wondered, was it possible to capture the elusive bird’s sound in the wild to find out if any individuals are left?

    It’s not an unheard-of idea. Scientists have used bioacoustics — a subfield of ecology that relies on sound to make environmental analyses — for everything from recording dolphins’ communication patterns to studying bats from afar to avoid virus spillover from humans (SN: 12/7/17; SN: 10/23/22). With artificial intelligence, it is now possible to use large audio datasets to train algorithms to spot different animal sounds within the cacophony of a natural background.

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    But the problem is that recordings of the purple-winged ground dove singing are as rare as the bird itself.

    “I came across [the bird’s song] watching a 1985 interview with Carlos Keller, a former bird breeder in São Paulo state, who had a few individuals of the dove,” says Carlos Araújo, an ecologist at the Instituto de Biología Subtropical at the Universidad Nacional de Misiones in Argentina. “And they sang while he spoke.”

    With Keller’s help, Araujo and colleagues accessed the decades-old recording and isolated the bird’s song.

    The next challenge was to see if it was even possible to identify individual bird songs amidst the sounds of other birds chirping, leaves rustling, rain falling, insects whirring and gnawing and larger animals moving through the forest.

    “We took a step back and did some analyses with other birds that are critically endangered but there are known individuals,” Araújo says. The team focused on three species found in Foz do Iguaçu, a national park that straddles the border of Brazil and Argentina: the cherry-throated tanager (Nemosia rourei), the Alagoas antwren (Myrmotherula snowi) and the blue-eyed ground-dove (Columbina cyanopis). These birds live in the same environments as the purple-winged ground dove. And the blue-eyed ground dove’s story inspires hope: The species went missing in 1941 and was rediscovered in 2016.

    To test their setup, the researchers looked for the cherry-throated tanager (shown) and two other rare birds.Ben Phalan/Parque das Aves

    The researchers installed 30 recorders in strategic spots along green areas in the Brazilian part of Foz do Iguaçu and recorded from July 2021 to April 2022. They also used data from another 100 recorders on the Argentinian side of Foz.

    “We went looking for the Guadua trinii bamboo to place the recorders,” says Benjamin Phalan, Head of Conservation at Parque das Aves, a private institution in Foz do Iguaçu focused on the conservation of Atlantic Forest birds. Like the purple-winged ground dove, the three bird species follow the flowering season of the G. trinii bamboo, which happens about once every 30 years.

    The team pushed through thickets of bamboo, braved ticks and biting flies, and watched out for venomous snakes such as jacaracas pit vipers. Bumping into these snakes is “rare but can happen. So we use galoshes or gaiters to protect us in case anyone steps on a snake or near it,” Phalan says.

    Carlos de Araujo installs a recording device in a South American forest. He and colleagues hope to pluck the song of rare birds out of the forest sounds the device picks up. Ben Phalan/Parque das Aves

    The recorders captured one minute of landscape sound every 10 minutes and generated about 3,000 days’ worth of recordings. “A lot of data to sift through,” says Araújo.

    Readily available analysis software wouldn’t work. These software, Araújo says, “need a lot of data input. With such rare species, we just don’t have that much data to train the identification algorithm.”

    So the team started from scratch, working with the little data they had for the three endangered birds. First, Araújo created a signal template — exactly like the birds’ singing — based on just a few recordings. The algorithm then compares that template with the soundscape recordings, separating signal from noise. If it spots a sound that is similar to the template, chances are that it is the bird that the researchers are looking for.

    The method relies on a statistical model “that is not new, but was used in a very clever and unusual way,” says David Donoso, an ecosystem ecology researcher at the Technische Universität Darmstadt in Germany. Donoso and colleagues recently used bioacoustics to investigate the recovery of Choco, a biodiversity hot spot in Ecuador that had been transformed in an agricultural area.

    There are different approaches to bioacoustics depending on what you’re looking for, Donoso says. “You can either use fewer recordings to map a whole animal soundscape to tell what species are there, like we did, or you can use lots of recordings to look for a single sound pattern,” he says. The study at Foz do Iguaçu “shows that you can use a relatively simple model to answer a complex question — and it works.”

    The tool worked reasonably well to identify the cherry-throated tanager and blue-eyed ground-dove singing, but not so much for the Alagoas antwren, Araújo’s team reports October 23 in Bioacoustics. “We’re trying to understand what happened, but we know that the algorithm works,” he says.

    The next step, Araújo says, is to refine the algorithm’s precision to find the Alagoas antwren and train it to look for the purple-winged ground dove. And they will do so at the same time. “We’re aiming at both goals at once because we’re running against the clock to find these birds,” Araújo says. “In the end, we are looking for a ghost.” But not a silent one, he hopes.  More

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    Capturing methane from the air would slow global warming. Can it be done?

    This summer was the hottest ever recorded on Earth, and 2023 is on track to be the hottest year. Heat waves threatened people’s health across North America, Europe and Asia. Canada had its worst wildfire season ever, and flames devastated the city of Lahaina in Maui. Los Angeles was pounded by an unheard-of summer tropical storm while rains in Libya caused devastating floods that left thousands dead and missing. This extreme weather is a warning sign that we are living in a climate crisis, and a call to action.

    Carbon dioxide emissions from burning fossil fuels are the main culprit behind climate change, and scientists say they must be reined in. But there’s another greenhouse gas to deal with: methane. Tackling methane may be the best bet for putting the brakes on rising temperatures in the short term, says Rob Jackson, an Earth systems scientist at Stanford University and chair of the Global Carbon Project, which tracks greenhouse gas emissions. “Methane is the strongest lever we have to slow global warming over the next few decades.”

    That’s because it’s relatively short-lived in the atmosphere — methane lasts about 12 years, while CO2 can stick around for hundreds of years. And on a molecule-per-molecule basis, methane is more potent. Over the 20-year period after it’s emitted, methane can warm the atmosphere more than 80 times as much as an equivalent amount of CO2.

    We already have strategies for cutting methane emissions — fixing natural gas leaks (methane is the main component of natural gas), phasing out coal (mining operations release methane), eating less meat and dairy (cows burp up lots of methane) and electrifying transportation and appliances. Implementing all existing methane-mitigation strategies could slow global warming by 30 percent over the next decade, research has shown.

    But some climate scientists, including Jackson, say we need to go further. Several methane sources will be difficult, if not impossible, to eliminate. That includes some human-caused emissions, such as those produced by rice paddies and cattle farming — though practices do exist to reduce these emissions (SN: 11/28/15, p. 22). Some natural sources are poised to release more methane as the world warms. There are signs that tropical wetlands are already releasing more of the gas into the atmosphere, and rapid warming in the Arctic could turn permafrost into a hot spot for methane-making microbes and release a bomb of methane stored in the currently frozen soil.

    So scientists want to develop ways to remove methane directly from the air.

    Three billion metric tons more methane exist in the atmosphere today than in preindustrial times. Removing that excess methane would cool the planet by 0.5 degrees Celsius, Jackson says.

    Similar “negative emissions” strategies are already in limited use for CO2. That gas is captured where it’s emitted, or directly from the air, and then stored somewhere. Methane, however, is a tricky molecule to capture, meaning scientists need different approaches.

    Most ideas are still in early research stages. The National Academies of Sciences, Engineering and Medicine is currently studying these potential technologies, their state of readiness and possible risks, and what further research and funding are needed. Some of the approaches include re-engineering bacteria that are already pros at eating methane and developing catalytic reactors to place in coal-mine vents and other methane-rich places to chemically transform the gas.

    “Methane is a sprint and CO2 is a marathon,” says Desirée Plata, a civil and environmental engineer at MIT. For scientists focused on removing greenhouse gases, it’s off to the races.

    Microbes already remove methane from the air

    Methane, CH4, is readily broken down in the atmosphere, where sunshine and highly reactive hydroxyl radicals are abundant. But it’s a different story when chemists try to work with the molecule. Methane’s four carbon-hydrogen bonds are strong and stable. Currently, chemists must expose the gas to extremely high temperatures and pressures to break it down.

    Even getting hold of the gas is difficult. Despite its potent warming power, it’s present in low concentrations in the atmosphere. Only 2 out of every 1 million air molecules are methane (by comparison, about 400 of every 1 million air molecules are CO2). So it’s challenging to grab enough methane to store it or efficiently convert it into something else.

    Nature’s chemists, however, can take up and transform methane even in these challenging conditions. These microbes, called methanotrophs, use enzymes to eat methane. The natural global uptake of methane by methanotrophs living in soil is about 30 million metric tons per year. Compare that with the roughly 350 million tons of methane that human activities pumped into the atmosphere in 2022, according to the International Energy Agency.

    Microbiologists want to know whether it’s possible to get these bacteria to take up more methane more quickly.

    Lisa Stein, a microbiologist at the University of Alberta in Edmonton, Canada, studies the genetics and physiology of these microbes. “We do basic research to understand how they thrive in different environments,” she says.

    Methanotrophs work especially slowly in low-oxygen environments, Stein says, like wetland muck and landfills, the kinds of places where methane is plentiful. In these environments, microbes that make methane, called methanogens, generate the gas faster than methanotrophs can gobble it up.

    But it might be possible to develop soil amendments and other ecosystem modifications to speed microbial methane uptake, Stein says. She’s also talking with materials scientists about engineering a surface to encourage methanotrophs to grow faster and thus speed up their methane consumption.

    Scientists hope to get around this speed bump with a more detailed understanding of the enzyme that helps many methanotrophs feast on methane. Methane monooxygenase, or MMO, grabs the molecule and, with the help of copper embedded in the enzyme, uses oxygen to break methane’s carbon-hydrogen bonds. The enzyme ultimately produces methanol that the microbes then metabolize.

    Boosting MMO’s speed could not only help with methane removal but also allow engineers to put methanotrophs to work in industrial systems. Turning methane into methanol would be the first step, followed by several faster reactions, to make an end product like plastic or fuel.

    Some bacteria, including Methylococcus capsulatus (shown), naturally break down methane with the enzyme methane monooxygenase. By studying the enzyme’s structure, scientists hope to speed up bacteria’s uptake of the greenhouse gas.Anne Fjellbirkeland/Wikimedia Commons (CC BY 2.5)

    “Methane monooxygenases are not superfast enzymes,” says Amy Rosenzweig, a chemist at Northwestern University in Evanston, Ill. Any reaction involving MMO will impose a speed limit on the proceedings. “That is the key step, and unless you understand it, it’s going to be very difficult to make an engineered organism do what you want,” Rosenzweig says.

    Enzymes are often shaped to fit their reactants — in this case, methane — like a glove. So having a clear view of MMO’s physical structure could help researchers tweak the enzyme’s actions. MMO is embedded in a lipid membrane in the cell. To image it, structural biologists have typically started by using detergents to remove the lipids, which inactivates the enzyme and results in an incomplete picture of it and its activity. But Rosenzweig and colleagues recently managed to image the enzyme in this lipid context. This unprecedented view of MMO in its native state, published in 2022 in Science, revealed a previously unseen site where copper binds.

    But that’s still not the entire picture. Rosenzweig says she hopes her structural studies, along with other work, will lead to a breakthrough soon enough to help forestall further consequences of global warming. “Maybe people get lucky and engineer a strain quickly,” Rosenzweig says. “You don’t know until you try.”

    Chemists make progress on catalysts

    Other scientists seek to put methane-destroying chemical reactors close to methane sources. These reactors typically use a catalyst to speed up the chemical reactions that convert methane into a less planet-warming molecule. These catalysts often require high temperatures or other stringent conditions to operate, contain expensive metals like platinum, and don’t work well at the concentrations of methane found in ambient air.

    One promising place to start, though, is coal mines. Coal mining is associated with tens of millions of tons of methane emissions worldwide every year. Although coal-fired power plants are being phased out in many countries, coal will be difficult to eliminate entirely due to its key role in steel production, says Plata, of MIT.

    To develop a catalyst that might work in a coal mine, Plata found inspiration in MMO. Her team developed a catalyst material based on a silicate material embedded with copper — the same metal found in MMO and much less expensive than those usually required to oxidize methane. The material is also porous, which improves the catalyst’s efficiency because it has a larger surface area, and thus more places for reactions to occur, than a nonporous material would. The catalyst turns methane into CO2, a reaction that releases heat, which is needed to further fuel the reaction. If methane concentrations are high enough, the reaction will be self-sustaining, Plata says.

    Turning methane into CO2 may sound counterproductive, but it reduces warming overall because methane traps much more heat than CO2 and is far less abundant in the atmosphere. If all the excess methane in the atmosphere were turned into CO2, according to a 2019 study led by Jackson, it would result in only 8.2 billion additional tons of CO2 — equivalent to just a few months of CO2 emissions at today’s rates. And the net effect would be to lessen the heating of the atmosphere by a sixth.

    Cattle feedlots are another place where Plata’s catalytic reactor might work. Barns outfitted with fans to keep cattle comfortable move air around, so reactors could be fitted to these ventilation systems. The next step is determining whether methane concentrations at industrial dairy farms are high enough for the catalyst to work.

    At Drumgoon Dairy in South Dakota, Elijah Martin (left) and Will Sawyer (right) test a small-scale thermal catalytic unit developed in Desirée Plata’s lab at MIT. The reactor transforms methane into carbon dioxide, which could lower the planet’s net warming rate because methane is a stronger greenhouse gas.D. Plata

    Another researcher making progress is energy scientist and engineer Arun Majumdar, one of Jackson’s collaborators at Stanford. In January, Majumdar published initial results describing a catalyst that converts methane into methanol, with an added boost from high-energy ultraviolet light. This UV blast adds the energy needed to overcome CH4’s stubborn bonds — and the carefully designed catalyst stays on target. Previous catalyst designs tended to produce a mix of CO2 and methanol, but this catalyst mostly sticks to making methanol.

    Is geoengineering a path to methane removal?

    A more extreme approach to speed up methane’s natural breakdown is to change the chemistry of the atmosphere itself. A few companies, such as the U.S.-based Blue Dot Change, have proposed releasing chemicals into the sky to enhance methane oxidation.

    Natalie Mahowald, an atmospheric chemist at Cornell University, decided to evaluate this type of geoengineering.

    “I’m not super excited about throwing more things into the atmosphere,” Mahowald says. To meet the goals of the Paris Agreement, limiting global warming to 1.5 to 2 degrees Celsius above the preindustrial average, though, it’s worth exploring all possibilities, she says. “If we’re going to meet these targets,” she says “we’re going to need some of these crazy ideas to work. So I’m willing to look at it. But I’m looking with a scientist’s critical eye.”

    The main strategy proposed by advocates would inject iron aerosols into the air over the ocean on a sunny day. These aerosols would react with salty sea spray aerosols to form chlorine, which would then attack methane in the atmosphere and initiate further chemical reactions that turn it into CO2. Mahowald wondered how much chlorine would be needed — and if there might be any unintended consequences.

    Detailed modeling revealed something alarming. The iron injections could have the opposite of the intended effect, Mahowald and colleagues reported in July in Nature Communications. Chlorine won’t attack methane if ozone is around. Instead, chlorine will first break down all the ozone it can find. But ozone plays a key role in generating the hydroxyl radicals that naturally break down atmospheric methane. So when ozone levels fall, Mahowald says, the concentration and lifetime of methane molecules in the atmosphere actually increases. To use this strategy to break down methane, geo­engineers would need to add a tremendous amount of chlorine to the atmosphere — enough to first break down the ozone, then attack methane.

    Removing 20 percent of the atmosphere’s methane, thus reducing the planet’s surface temperature by 0.2 degrees Celsius by 2050, for example, would require creating about 630 million tons of atmospheric chlorine every year. That would in turn require injecting perhaps tens of millions of tons of iron. A form of particulate matter, these iron aerosols could worsen air quality; inhaling particulate matter is associated with a range of health problems, particularly cardiovascular and lung disease. This atmospheric tinkering could also create hydrochloric acid that could reach the ocean and acidify it.

    And there’s no guarantee that some of the chlorine wouldn’t make it all the way up to the ozone layer, depleting the planetary shield that protects us from the sun’s harmful UV rays. Mahowald is still studying this possibility.

    Methane is a sprint and CO2 is a marathon. Desirée Plata

    Mahowald is ambivalent about doing research on geoengineering. “We’re just throwing out ideas here because we’re in a terrible, terrible position,” she says. She’s worried about what could happen if all the methane locked up in the world’s permafrost escapes. If scientists can figure out how to use iron aerosols effectively, without adverse effects — and if such geoengineering is accepted by society — we might need it.

    “We’re just trying to see, is there any hope this could work and would we ever want to do it? Would it have enough benefits to outweigh the disadvantages?”

    The committee organized by the National Academies to investigate methane removal is taking these kinds of ethical questions into account, as well as considering the potential cost and scale of technologies. Stein, a committee member, says a framework proposed by Spark Climate Solutions provides some guidance. The organization, a nonprofit based in San Francisco that evaluates methane-removal technologies, proposes investing in tech that can remove tens of millions of tons of methane per year in the coming decades, at a cost of less than $2,000 per ton. Spark cofounder David Mann says the numbers are designed to focus attention and investment on technologies that can make a real difference in curbing climate change in the near term.

    The National Academies group aims to make recommendations about research priorities on methane-removal technologies by next summer. It’s likely that a portfolio of different technologies will be necessary. What works in a cattle feedlot may not work at a wastewater treatment plant, for instance.

    Scientists focused on methane removal are eager for more researchers, research funding and companies to enter the fray — and quickly. “It’s been a crazy year,” Jackson says of 2023’s extreme weather. We’re already feeling the effects of global warming, but we can seize the moment, he says. “This problem is not something for our grandchildren. It’s here.” More

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    Reindeer herders and scientists collaborate to understand Arctic warming

    The spring 2014 annual reindeer festival in Yar-Sale, a rural town on the Yamal Peninsula in Western Siberia, was a grim affair. A rainstorm followed by a deep freeze the previous November had turned the normally snow-covered tundra into an ice shield. Reindeer could not paw through the thick ice to access lichen, their primary food source. In a region where winter temperatures can plunge below –50° Celsius, that ground remained frozen months later. Tens of thousands of reindeer had already died of starvation. Thousands more were on the brink of death.

    A prominent reindeer herder named Vasily Serotetto approached a group of scientists. Could they predict when such an event — known as seradt in the Indigenous Nenets language — might occur, he asked. Even a few days advance notice would have enabled mobile slaughterhouse operators to come in and humanely kill the animals. And the animal meat and fur would not have gone to waste.

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    To the scientists in attendance, the request felt like a call to action. Serotetto was basically saying: “You scientists, what’s causing this?” says Bruce Forbes, a biogeographer at the University of Lapland in Rovaniemi, Finland.

    The scientists possessed a trove of satellite images of the Russian Arctic to start tackling that question, Forbes knew. But without more detailed, on-the-ground information from local inhabitants, such as the timing of the event and where it occurred, they did not know where to begin looking in that massive amount of data.

    Now the two groups have joined forces to try to understand a phenomenon that has crucial implications for a people’s way of life, as well as a world at large grappling with climate change. Besides preventing herbivores from accessing foliage underneath the ice, rain on snow has been shown to trigger slush avalanches, create surface conditions that warm permafrost, change soil and vegetation conditions and disrupt transportation and communications.

    While that paired knowledge helped unravel the many factors that caused the deadly icing in 2013, finding a way to predict such events remains a puzzle.

    Power of partnership

    The idea that Indigenous and scientific communities can help each other has been gaining prominence in recent years. Forbes is part of a group of interdisciplinary scientists involved in the Arctic Rain on Snow Study, or AROSS, which is funded by the National Science Foundation. The team is studying what causes rain on snow in the Arctic and how such events affect local wildlife, ecology and communities.

    And in September, NSF launched a research hub, the Center for Braiding Indigenous Knowledges and Science. That $30-million, five-year effort to bridge Western and Indigenous ways of knowing is based at the University of Massachusetts Amherst.

    Indigenous people, such as the Siberian reindeer herders, have a deep understanding of their local environs, says linguistic anthropologist Roza Laptander, an AROSS team member originally from the Yamal Peninsula. Laptander, of both the University of Lapland and the University of Hamburg in Germany, has periodically embedded with herding communities since 2006.

    Laptander’s research shows how ecological knowledge is encoded in the Nenets language. For instance, the first snow of the season is often soft and deep, or idebya syra, Laptander reported in September in Ecology and Society. That snow is difficult for the reindeer to walk in. Snow with ice granules, or inggyem’ syra, indicates high-quality lichen. Seradt, caused by rain falling on snow or unfrozen ground and then freezing solid, is to be feared. The word stems from serad’’, which translates to both rain and misfortune.

    Every winter, reindeer herders migrate across Western Siberia’s Yamal Peninsula in search of the animals’ main food source, lichen. Warming Arctic temperatures have increased the likelihood that rain will fall on snow, and then freezing temperatures will bury lichen under thick ice — which occurred in 2013. That winter, over 61,000 reindeer starved to death.Roza Laptander

    Historically, the herders could rely on their in-depth knowledge of varying types of snow and ice, along with an ability to read weather patterns and animal behavior, to gauge the likelihood of a difficult winter, Laptander says. But a rapidly warming Arctic is scrambling those signals. “Their traditional ways of predicting weather do not work anymore,” she says.

    Scientists, meanwhile, often look to understand how warming-fueled changes to the Arctic climate, such as thinning sea ice and melting permafrost, are affecting climate change and weather patterns on a global scale (SN: 8/31/23). Knowing where to zoom in and what to zoom in on to help local communities requires those communities’ input.

    “[Scientists] probably wouldn’t even know one type of snow is different than another. We might just look and say, ‘There’s snow here,’” says Dylan Davis, a remote sensing archaeologist at Columbia University who is not involved with this project. “Local communities and Indigenous communities that live with this every day, they’re going to be able to see things that we don’t.”

    Prediction challenges

    That’s what happened at Yar-Sale. Forbes told Serotetto that scientists might be able to sort out what caused the 2013–14 seradt, but they needed an idea of where to begin. Serotetto pointed to a map. In a typical winter, herders migrate from north to south. When the rain-on-snow event hit, many herders were already too far south to turn back or doubted the severity of the disaster. Serotetto, a herder with decades of experience, was able to push north. He discovered that the northern peninsula was relatively unscathed.

    Serotetto drew a line on the map demarcating where he had come across the edge of the ice shield. When scientists pulled up satellite images from that November day, Forbes says, “the line was exactly where he drew it.” 

    That information enabled Laptander, Forbes and others on the team to begin investigating the unique confluence of sea ice levels, snow versus ice cover on land, air temperatures and precipitation that contributed to the November 2013 icing event in southern Yamal.

    Melting sea ice in the Barents and Kara seas releases humid air into the atmosphere, the team found (SN: 11/15/16). That humid air can blow onto the land as rain when temperatures rise above freezing.

    The answer to Serotetto’s question, though, is far from resolved. Predicting such events remains extremely challenging, Forbes says. For instance, in 2018, the North Atlantic was open water all the way to the North Pole, and rain-on-snow seemed almost inevitable. But such an event did not occur. How did conditions differ between 2013 and 2018?

    Efforts to answer that question are currently on hold. First, the pandemic thwarted travel and then, in February 2022, Russia invaded Ukraine. Climate research in the Russian Arctic has come to a virtual standstill, Forbes says. “Suddenly, half the Arctic is a no-go.”  

    But the work in Yamal has snowballed to other Arctic regions, Forbes says. For instance, on a trip to Greenland last year, sheep farmers and reindeer herders told Forbes that they had just dealt with their first serious rain-on-snow event the previous winter. Forbes and his colleagues are hoping to apply what they learned in Yamal to better understand that event. “Now we have a data-sharing network with Indigenous informants across Arctic North America,” Forbes says. More

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    Crabs left the sea not once, but several times, in their evolution

    Most terrestrial plants and animals left the ocean a single time in their evolutionary history to live ashore. But crabs have seemingly scuttled out of the sea more than a dozen times, with at least two groups later reverting back to a marine lifestyle, a study finds.

    The research, published November 6 in Systematic Biology, sheds new light on the evolutionary history of the group Brachyura, which includes roughly 7,600 species of “true crabs,” and includes the most comprehensive evolutionary tree yet created for the group. And the study offers clues about how other early invertebrates may have evolved a terrestrial lifestyle, researchers say.

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    Unlike for well-studied animals such as birds and mammals, a unified crab tree of life has been lacking, says Kristin Hultgren, an invertebrate zoologist at Seattle University. “While the authors have developed a useful framework for understanding the complexity of transitioning to terrestrial life, one of the most important contributions is the extensive, well-dated evolutionary tree.”

    Crabs are an extremely diverse group and have colonized nearly every type of habitat on Earth. It’s been a challenge to study when crabs first shifted from one habitat to another during evolution because, like some other invertebrates, crabs don’t have the extensive fossil trail that early vertebrates do, says Joanna Wolfe, an evolutionary biologist at Harvard University.

    Past research has also often treated marine, freshwater and land crabs as discrete subgroups when they’re more like a continuum, Wolfe says. “They’re not distinct and actually have a lot in common, and looking at them together helps trace their evolution.”

    Wolfe and her colleagues collected genetic data from 333 species of crabs in the group Brachyura. These crustaceans are evolutionarily distinct from, although closely related to, another group of crustaceans that independently evolved crablike bodies and are often erroneously referred to as crabs, including animals like the hermit and king crabs.

    The team then combined that genetic data with dozens of fossils to generate a crab evolutionary tree, layering on details about each species’ life history and adaptations for living on land to reconstruct a possible timeline of when crabs colonized drier ground.

    True crabs diverged from other crustacean lineages roughly 230 million years ago during the Triassic Period, the researchers found, refining previous estimates. Over the next hundred or so million years, brachyurans diversified widely during a period previously dubbed the “Cretaceous crab revolution.”

    The study also showed that during their evolution, crabs appear to have adapted to a more terrestrial lifestyle as many as 17 times, either by shifting from the ocean to the intertidal zone or similarly salty habitats like mangroves, or by colonizing freshwater estuaries and rivers on route to land. In at least two cases, crabs reverted to a marine lifestyle long after they’d left.

    The amount of times that crabs independently left the ocean is “astonishing,” says Katie Davis, an evolutionary paleobiologist at the University of York in England who was not involved in the research. “And it’s really fantastic that molecular biology, fossils and modern numerical techniques can be combined to provide insight into previously unanswerable questions.”

    The study also hints at what other early arthropods that ventured onto the land may have been like, Wolfe says. Past studies have shown that crabs and insects share a common, if unknown, aquatic ancestor. By looking at the types of crabs that successfully left the ocean, it’s possible to guess at what adaptations early insects might have needed to do the same. Modern crabs living out of the water today, for example, excel at keeping themselves from drying out and have limited their dependence on water for reproduction.

    “If you’re going to be the first proto-insect to come out of the ocean … you’re probably going to need those kinds of adaptations,” Wolfe says. More

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    Grassland and shrubland fires destroy more U.S. homes than forest fires

    Forest fires can devastate vast swaths of land, but in the United States, another category of conflagrations takes the title of most destructive.

    Of the homes destroyed in wildfires across the contiguous United States from 1990 to 2020, 64 percent — nearly 11,000 — were razed by grassland and shrubland fires, researchers report in the Nov. 10 Science.  

    “We often think about forest fires because that’s what we see on the news … they’re dramatic, they’re huge, they’re intense,” says ecologist Volker Radeloff of the University of Wisconsin-Madison, “but grassland and shrubland fires can also be quite destructive.” For instance, the 2023 Lahaina fire on the Hawaiian island of Maui, fueled by invasive wild grasses, killed at least 98 people and destroyed some 2,200 buildings.

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var(–zephr-typography-body-fallbackFont)}.zephr-registration-form-input-select.svelte-19a73pq{display:block;appearance:auto;width:100%;height:calc(var(–zephr-input-height) * 1px);font-size:16px;border:calc(var(–zephr-input-borderWidth) * 1px) solid var(–zephr-color-text-main);border-radius:calc(var(–zephr-input-borderRadius) * 1px);transition:border-color 0.25s ease, box-shadow 0.25s ease;outline:0;color:var(–zephr-color-text-main);background-color:#fff;padding:10px}.zephr-registration-form-input-select.disabled.svelte-19a73pq{border:1px solid var(–zephr-color-background-tinted)}.zephr-registration-form-input-select.unselected.svelte-19a73pq{color:var(–zephr-color-background-tinted)}.zephr-registration-form-input-select.error.svelte-19a73pq{border-color:var(–zephr-color-warning-main)}.zephr-registration-form-input-textarea.svelte-19a73pq{background-color:#fff;border:1px solid #ddd;color:#222;font-size:14px;font-weight:300;padding:16px;width:100%}.zephr-registration-form-input-slider-output.svelte-19a73pq{margin:13px 0 0 10px}.zephr-registration-form-input-inner-text.svelte-lvlpcn{cursor:pointer;position:absolute;top:50%;transform:translateY(-50%);right:10px;color:var(–zephr-color-text-main);font-size:12px;font-weight:bold;font-family:var(–zephr-typography-body-font), var(–zephr-typography-body-fallbackFont)}.spin.svelte-1cj2gr0{animation:svelte-1cj2gr0-spin 2s 0s infinite linear}.pulse.svelte-1cj2gr0{animation:svelte-1cj2gr0-spin 1s infinite steps(8)}@keyframes svelte-1cj2gr0-spin{0%{transform:rotate(0deg)}100%{transform:rotate(360deg)}}.zephr-registration-form-checkbox.svelte-1gzpw2y{position:absolute;opacity:0;cursor:pointer;height:0;width:0}.zephr-registration-form-checkbox-label.svelte-1gzpw2y{display:flex;align-items:center;font-family:var(–zephr-typography-body-font), var(–zephr-typography-body-fallbackFont)}.zephr-registration-form-checkmark.svelte-1gzpw2y{position:relative;box-sizing:border-box;height:23px;width:23px;background-color:#fff;border:1px solid var(–zephr-color-text-main);border-radius:6px;margin-right:12px;cursor:pointer}.zephr-registration-form-checkmark.checked.svelte-1gzpw2y{border-color:#009fe3}.zephr-registration-form-checkmark.checked.svelte-1gzpw2y:after{content:””;position:absolute;width:6px;height:13px;border:solid #009fe3;border-width:0 2px 2px 0;transform:rotate(45deg);top:3px;left:8px;box-sizing:border-box}.zephr-registration-form-checkmark.disabled.svelte-1gzpw2y{border:1px solid var(–zephr-color-background-tinted)}.zephr-registration-form-checkmark.disabled.checked.svelte-1gzpw2y:after{border:solid var(–zephr-color-background-tinted);border-width:0 2px 2px 0}.zephr-registration-form-checkmark.error.svelte-1gzpw2y{border:1px solid var(–zephr-color-warning-main)}.zephr-registration-form-input-radio.svelte-1qn5n0t{position:absolute;opacity:0;cursor:pointer;height:0;width:0}.zephr-registration-form-radio-label.svelte-1qn5n0t{display:flex;align-items:center;font-family:var(–zephr-typography-body-font), var(–zephr-typography-body-fallbackFont)}.zephr-registration-form-radio-dot.svelte-1qn5n0t{position:relative;box-sizing:border-box;height:23px;width:23px;background-color:#fff;border:1px solid #ebebeb;border-radius:50%;margin-right:12px}.checked.svelte-1qn5n0t{border-color:#009fe3}.checked.svelte-1qn5n0t:after{content:””;position:absolute;width:17px;height:17px;background:#009fe3;background:linear-gradient(#009fe3, #006cb5);border-radius:50%;top:2px;left:2px}.disabled.checked.svelte-1qn5n0t:after{background:var(–zephr-color-background-tinted)}.error.svelte-1qn5n0t{border:1px solid var(–zephr-color-warning-main)}.zephr-form-link.svelte-64wplc{margin:10px 0;color:#6ba5e9;text-decoration:underline;cursor:pointer;font-family:var(–zephr-typography-body-font), var(–zephr-typography-body-fallbackFont)}.zephr-form-link-disabled.svelte-64wplc{color:var(–zephr-color-text-main);cursor:none;text-decoration:none}.zephr-registration-form-google-icon.svelte-1jnblvg{width:20px}.zephr-registration-form-password-progress.svelte-d1zv9r{display:flex;margin-top:10px}.zephr-registration-form-password-bar.svelte-d1zv9r{width:100%;height:4px;border-radius:2px}.zephr-registration-form-password-bar.svelte-d1zv9r:not(:first-child){margin-left:8px}.zephr-registration-form-password-requirements.svelte-d1zv9r{margin:20px 0;justify-content:center}.zephr-registration-form-password-requirement.svelte-d1zv9r{display:flex;align-items:center;color:var(–zephr-color-text-tinted);font-size:12px;height:20px;font-family:var(–zephr-typography-body-font), var(–zephr-typography-body-fallbackFont)}.zephr-registration-form-password-requirement-icon.svelte-d1zv9r{margin-right:10px;font-size:15px}.zephr-registration-form-password-progress.svelte-d1zv9r{display:flex;margin-top:10px}.zephr-registration-form-password-bar.svelte-d1zv9r{width:100%;height:4px;border-radius:2px}.zephr-registration-form-password-bar.svelte-d1zv9r:not(:first-child){margin-left:8px}.zephr-registration-form-password-requirements.svelte-d1zv9r{margin:20px 0;justify-content:center}.zephr-registration-form-password-requirement.svelte-d1zv9r{display:flex;align-items:center;color:var(–zephr-color-text-tinted);font-size:12px;height:20px;font-family:var(–zephr-typography-body-font), var(–zephr-typography-body-fallbackFont)}.zephr-registration-form-password-requirement-icon.svelte-d1zv9r{margin-right:10px;font-size:15px}
    .zephr-registration-form {
    max-width: 100%;
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    font-family: var(–zephr-typography-body-font), var(–zephr-typography-body-fallbackFont);
    margin: 0px auto;
    margin-bottom: 4rem;
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    .zephr-registration-form-text h6 {
    font-size: 0.8rem;
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    .zephr-registration-form h4 {
    font-size: 3rem;
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    .zephr-registration-form h4 {
    font-size: 1.5rem;
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    border-color: #e04821;
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    margin-right: auto;
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    .zephr-registration-form-button.svelte-17g75t9 {
    background-color: #e04821;
    border-color: #e04821;
    width: 150px;
    margin-left: auto;
    margin-right: auto;
    }
    .zephr-registration-form-text > * {
    color: #FFFFFF;
    font-weight: bold
    font: 25px;
    }
    .zephr-registration-form-progress-bar.svelte-8qyhcl {
    width: 100%;
    border: 0;
    border-radius: 20px;
    margin-top: 10px;
    display: none;
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    .zephr-registration-form-response-message-title.svelte-179421u {
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    background-color: #8db869;
    border: 1px solid #8db869;
    color: white;
    margin-top: -0.2rem;
    }
    .zephr-registration-form-text.svelte-i1fi5:nth-child(1){
    font-size: 18px;
    text-align: center;
    margin: 20px auto;
    font-family: var(–zephr-typography-body-font), var(–zephr-typography-body-fallbackFont);
    color: white;
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    .zephr-registration-form-text.svelte-i1fi5:nth-child(5){
    font-size: 18px;
    text-align: left;
    margin: 20px auto;
    font-family: var(–zephr-typography-body-font), var(–zephr-typography-body-fallbackFont);
    color: white;
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    .zephr-registration-form-text.svelte-i1fi5:nth-child(7){
    font-size: 18px;
    text-align: left;
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    font-family: var(–zephr-typography-body-font), var(–zephr-typography-body-fallbackFont);
    color: white;
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    .zephr-registration-form-text.svelte-i1fi5:nth-child(9){
    font-size: 18px;
    text-align: left;
    margin: 20px auto;
    font-family: var(–zephr-typography-body-font), var(–zephr-typography-body-fallbackFont);
    color: white;
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    color: white;
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    border: calc(var(–zephr-input-borderWidth) * 1px) solid var(–zephr-input-borderColor);
    background-color: white;
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    .zephr-registration-form-checkbox-label.svelte-1gzpw2y {
    display: flex;
    align-items: center;
    font-family: var(–zephr-typography-body-font), var(–zephr-typography-body-fallbackFont);
    color: white;
    font-size: 20px;
    margin-bottom: -20px;
    }

    For the new study, Radeloff and his colleagues analyzed three decades of data on wildfire occurrence, land use and housing, hoping to learn more about what factors fuel such destructive blazes.

    The team found that about 337,000 square kilometers of grasslands and shrublands burned from 1990 to 2020, compared with about 144,000 square kilometers burned by forest fires. Though forest fires were about twice as likely as grassland fires to burn down homes they encountered, the much larger expanse burned by grassland and shrubland fires helped make them more destructive overall.

    The data also revealed that U.S. wildfire risk had risen substantially. Today, roughly 148,000 houses stand in areas where wildfires have burned before — that’s more than twice as many as in 1990. About half of those additional homes were built on land that had already burned prior to 1990, the team found, while the rest were already standing when a blaze burned through.

    Radeloff hopes more people will consider their wildfire risk and take steps to prepare, be that planning evacuation routes or fireproofing their homes. Evading wildfire danger, it seems, takes more than getting out of the woods. More