Environment

Forget Arizona or Florida — sun worshippers ought to head to the Atacama Desert in South America. It’s there that the sun’s rays on Earth are most intense, beating out places like Mount Everest and even, occasionally, rivaling the conditions on Venus, researchers report July 3 in the Bulletin of the American Meteorological Society.

Satellite data have suggested that the Altiplano — a high-altitude plateau in the Atacama that straddles parts of Chile, Bolivia, Peru and Argentina — experiences the most intense levels of sunlight on Earth. But since satellites look down on our planet’s surface from afar, it’s important to verify that claim with on-the-ground data, says Raúl Cordero, a physicist at the University of Santiago in Chile. “How good are these estimates?”

To answer that question, Cordero and colleagues set up a small atmospheric observatory, housed in two shipping containers, in the Chilean Altiplano. Since 2016, the researchers have been measuring solar radiation levels at the site using a pyranometer, a palm-sized instrument sensitive to ultraviolet, visible and near-infrared light.

A researcher working high in the Andes Mountains of Chile sets up an instrument to measure solar radiation.R. Cordero

Based on the first five years of data from the observatory, the average amount of solar power hitting each square meter of the landscape — 308 watts — is consistent with the earlier satellite observations and even higher than values recorded by a pyranometer near the summit of Mount Everest, the team reports.

The researchers also captured bursts of extremely intense solar radiation. One event, in January 2017, blasted the site with 2,177 watts per square meter — more than seven times the average. The intensity of that burst and others like it rivals solar radiation on Venus, which is over 40 million kilometers closer to the sun than Earth is (SN: 2/13/18). Such events, which typically last just a few minutes, are caused by thin clouds scattering light toward the ground, the researchers suggest. More

Utah’s trademarked “greatest snow on earth” may be getting dirtier — and melting faster — due in part to dust blowing off newly exposed lakebed from the shrinking Great Salt Lake.

Snow in the Wasatch Mountains above Salt Lake City had more dust deposited on it in 2022 than in any year since observations began in 2009, researchers report in the June Environmental Research Letters. The dust accumulation caused snow to disappear 17 days earlier than if the snow had been clean.

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An earlier, faster snowmelt may alter the water supply for the 1.2 million people who live in the region, as well as ecosystems downstream, says McKenzie Skiles, a snow hydrologist at the University of Utah in Salt Lake City. It also affects the region’s ski areas, which contribute more than $1.5 billion per year to the local economy.

In arid parts of the western United States, snow acts as a natural reservoir. More than half the municipal water in Salt Lake City comes from four streams that drain snow out of the Wasatch Mountains. But current forecasting tools don’t account for the impact of dust, Skiles says, which absorbs sunlight, speeding up snowmelt. That means people can’t accurately predict when snow runoff will happen so they can use water efficiently.

As an avid skier, Skiles noticed the slopes near Salt Lake City looked especially dirty in 2022. So she and colleagues investigated whether the increase in dust was related to consecutive years of record-low water in the Great Salt Lake (SN: 4/17/23).

The team collected snow samples from a plot adjacent to Alta Ski Resort and found that storms deposited substantial amounts of dust 16 times during the 2022 snowmelt season. After calculating where the dust came from during each storm based on wind direction and atmospheric conditions, the team found that Great Salt Lake contributed nearly a quarter of the total dust to the study site. It also released the most dust relative to the lake’s exposed surface area. This was surprising, Skiles says, because the Great Salt Lake’s dry lakebed is tiny compared with the exposed surfaces of neighboring dust sources, such as the much bigger West Desert, a dry landscape west of Great Salt Lake. The West Desert contributed about of half the dust, while other dried-up lakebeds and deserts, some as far away as Idaho and Nevada, delivered the rest.

A record amount of dust coated snow at the Atwater Study Plot near Alta, Utah, in spring of 2022. The dust speeded up snowmelt by 17 days.Otto Lang

“The future of Utah is going to be drier,” says Patrick Belmont, a hydrologist at Utah State University in Logan who was not part of the study. Earlier snowmelt causes the landscape to dry out faster, creating “a feedback loop that’s hard to break out of,” he explains. As Great Salt Lake shrinks and deposits more dust on the mountains, there’s less water available to refill the lake during the summer, which in turn exposes a larger dust source as the shoreline recedes.

A smaller lake also means less winter snow, Belmont says, as evaporation from Great Salt Lake contributes up to 10 percent of the snowpack in the Wasatch range. “Unless we make some big policy changes, we should expect to see a much lower Great Salt Lake, and it’s very possible that we lose the lake altogether.”

Skiles and her colleagues plan to keep monitoring the snowpack and to use remote sensing to see if dust is impacting snow across all of the mountains that drain into the Great Salt Lake. “We need more years of data to understand if this is the new normal,” she says. More

Hidden flows of water are poised to flush toxic contamination into U.S. coastal communities.

Sea level rise from climate change won’t just force shorelines to retreat — in inland areas, it will guilefully lift groundwater into shallower soils. That rising water could infiltrate hundreds of U.S. Superfund sites — severely polluted locations identified by the Environmental Protection Agency for cleanup — researchers warn in a preliminary study posted May 25 to ESS Open Archive.

These sites — and thousands of other polluted areas — could be at risk of releasing heavy metals, radioactive elements, pesticides and industrial chemicals associated with human health problems (SN: 4/26/23). People of color and low-income communities would be disproportionately affected.

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“Just the sheer number of Superfund sites where there are these dangerous contaminants that could be liberated — it’s astonishing,” says coastal geologist Patrick Barnard of the U.S. Geological Survey in Santa Cruz, Calif., who wasn’t involved in the study. Many of the polluted areas have been managed without regard for groundwater rise, he says. “We need to think about what the future holds for these sites.”

The link between climate change, the sea and underground water may not be obvious, but it is intimate. At the beach, seawater can seep into the ground and move inland, permeating layers of earth under coastal communities. Meanwhile, rain and runoff can also trickle down from above. In the ground, this freshwater often sits atop the denser saltwater from the sea. And when the sea level rises due to climate change, it pushes all this groundwater up through the earth (SN: 10/29/19).

As the top of the groundwater — the water table — nears the surface, it can damage human infrastructure. It can also spread hazardous substances in the soil, exposing people and ecosystems nearby.

Environmental planner and geologist Kristina Hill found motivation for the new study while investigating groundwater conditions at a former Superfund site in the San Francisco Bay Area. There, groundwater was touching pollutants in the soil. “I started wondering, what is the scale of this problem?” says Hill, of the University of California, Berkeley.

She and her colleagues identified which of the roughly 1,300 U.S. Superfund sites are in low-lying coastal areas — no more than 10 meters above mean sea level — where groundwater rise could potentially infiltrate.

They found if the sea surface rose by one meter — a possibility by 2100 — then groundwater could potentially rise into contaminated soils at 326 sites. New Jersey and Florida respectively contained the most at-risk Superfund sites — 54 and 51 respectively.

Not every polluted site in the United States is a Superfund site, but that doesn’t make them less hazardous, Hill says. Her team assessed that potential impact with a case study of the Bay Area alone. They flagged five Superfund sites and nearly 5,300 state-managed contaminated areas vulnerable to that one-meter sea level rise. There could be thousands more such sites up and down our coastlines, Hill says.

The researchers analyzed U.S. Census data to investigate who could face the greatest risk of exposure. People from socially vulnerable communities — those whose circumstances limit their ability to prevent suffering or loss in face of a disaster — bore disproportionate risk, they found.

“The findings are not surprising,” says hydrogeologist Holly Michael of the University of Delaware in Newark. This study takes the first step in addressing the hazard, by calling out where it could arise, she says. More local research will be needed to thoroughly assess each site’s risk and determine next steps, be that treating contaminated soils or removing them altogether.

As the ocean encroaches, Hill says, helping people move inland won’t be enough unless we also clean up our mess. “Otherwise, there will be a toxic area that we leave behind, and that will spread.” More

Some forests take one-two punches surprisingly well.

Researchers have shown that certain California forests exposed to two successive droughts weathered the second one much better than forests only hit by the later dry period. Given that the frequency and severity of droughts is increasing with climate change (SN: 3/10/22), the findings suggest that forested regions might fare better than predicted in the future, the research team proposes in the May 17 AGU Advances. That’s important because of the many resources that forests provide, including their ability to sequester about a quarter of the carbon dioxide that humans put into the atmosphere every year.

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Carl Norlen and Mike Goulden, ecologists at the University of California, Irvine, studied roughly 520,000 hectares of California forest (about 4 percent of the state’s forested areas). The researchers focused on conifers, trees such as pines and firs that have needles rather than flat leaves. Using archival data gleaned from airplane observations, Norlen and Goulden estimated the extent of conifer die-off during two droughts that struck from 1999–2002 and 2012–2015. “Both of them when they happened were considered some of the most severe droughts ever in California,” Norlen says.

When the researchers looked at forests that just experienced the 2012–2015 drought, they found that over 50 percent of forested areas showed evidence of die-off. But when Norlen and Goulden analyzed forests that had weathered both droughts, they were surprised to find that only 13 percent of those forested areas showed evidence of die-off after the second drought. The researchers also analyzed satellite data that revealed the severity of tree die-off, and they again found that forests hurt by one drought were better prepared to weather another.

The underlying cause of those differences probably has to do with the tree mortality that occurred during the first drought, Norlen and Goulden propose. Roughly 31 percent of the forested areas that experienced both droughts showed signs of die-off during the 1999–2002 drought. “We think that it has to do with experiencing die-off the first time,” Norlen says.

That makes sense, says William Anderegg, an ecologist at the University of Utah in Salt Lake City who was not involved in the research. “You might have culled out the weak trees,” he says.

Norlen and Goulden speculate that the first drought eliminated trees weakened by pests like bark beetles (SN: 2/21/23), or perhaps that the dry conditions prompted trees to protect themselves by growing deeper roots. Those changes would have helped protect the remaining trees from future droughts, Goulden says. “You effectively have a stronger population.”

Getting at the root of why exactly some forests are better prepared to weather successive droughts will require more investigation, the researchers say. One way forward is to monitor individual trees to better understand their physiology, which other teams have done by outfitting trees with sensors (SN: 4/25/23).

However, the new findings already provide some hope for the forests of the future. Modeling work has suggested that upwards of 50 percent of present-day conifer tree coverage could be lost in the Northern Hemisphere by the end of the century. But this new work shows that that prediction might well turn out to be an overestimate. “There’s an element of it that’s actually hopeful,” Goulden says. More

Meet the house that diapers built.

Researchers have designed and erected a house that has shredded, disposable diapers mixed into its concrete and mortar. A single-story home of about 36 square meters can pack nearly 2 cubic meters of used diapers into its floors, columns and walls, the team reports May 18 in Scientific Reports.

Using recycled diapers as composite building materials would not only shrink landfill waste but also could make such homes more affordable, the team says, a particular need in developing countries like Indonesia where the demand for low-cost housing far outstrips the supply.

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Indonesia’s urban population has increased by about 4 percent per year in the last three decades, and more of its people are moving to urban centers. Over two-thirds of Indonesians are expected to live in urban areas by 2025, says environmental engineer Siswanti Zuraida of the University of Kitakyushu in Japan. That population boom is putting a heavy strain on both housing demand and waste management, says Zuraida, who is originally from Indonesia. Used disposable diapers mostly pile up in landfills or get incinerated, adding to a growing waste problem.

The materials used to build a house, meanwhile, particularly those needed to shore up its structural integrity, are often the biggest barrier to making homes affordable. So researchers have previously examined the possibility of using a wide variety of unconventional materials that could also save costs. These materials included many that would otherwise pile up as waste, such as the husks of rice grains or fly ash, the fine residue left over from the combustion of pulverized coal. Disposable diapers, as it happens, contain a lot of potentially useful building material, such as wood pulp, cotton, rayon and plastic.

Zuraida and colleagues assessed how much of the sand, gravel and other traditional building materials used in mortar and concrete could be replaced by diapers — washed, dried, sterilized and shredded — without reducing the strength of the structures. They created six different samples of concrete and mortar by mixing different proportions of diaper material with cement, sand, gravel and water. Crushing the samples in a machine let the researchers test how much weight each could bear.

The team then went on to design — and then build — a small, single-story, two-bedroom, one-bathroom home based on the maximum amount of diaper waste they calculated they could use. Recycled diapers could replace up to 27 percent of the traditional materials used in load-bearing structural components like columns and beams without losing significant strength, the team found. For buildings with more floors, that fraction is somewhat less: A three-story home could use up to 10 percent disposable diapers in its load-bearing structures, the team calculated. As for nonstructural components like wall partitions or garden paving blocks, shredded diapers could replace up to 40 percent of the sand.

Despite the need for more affordable housing, there are significant hitches that stand in the way of adopting diapers or other low-impact nonconventional materials, Zuraida says.

Diapers’ plastic components would have to be separated from the organic fibers, a complicated recycling process currently available only in developed nations. And Indonesia’s building regulations restrict construction materials to concrete, bricks, wood and ceramics — materials that also bear a high cost in terms of carbon emissions.

“Thinking about how to use waste for other purposes is an excellent idea,” says chemist Christof Schröfl of Technische Universität Dresden in Germany. But there may be limits on the ultimate environmental friendliness of repurposing used diapers in buildings, he says, due to the existing challenges of separating and sanitizing diapers in waste. “It’s maybe worthwhile to start thinking about ways to replace single-use diapers” with something less frequently disposed of. More

When a strong tornado roars through a city, it often leaves behind demolished buildings, broken tree limbs and trails of debris. But a similarly powerful storm touching down over barren, unvegetated land is much harder to spot in the rearview mirror.

Now, satellite imagery has revealed a 60-kilometer-long track of moist earth in Arkansas that was invisible to human eyes. The feature was presumably excavated by a tornado when it stripped away the uppermost layer of the soil, researchers report in the March 28 Geophysical Research Letters. This method of looking for “hidden” tornado tracks is particularly valuable for better understanding storms that strike in the winter, when there’s less vegetation, the researchers suggest. And recent research has shown that wintertime storms are likely to increase in intensity as the climate warms (SN: 12/16/21).

Over 1,000 tornadoes strike the United States each year, according to the National Weather Service. But not all are equally likely to be studied, says Darrel Kingfield, a meteorologist at the National Oceanic and Atmospheric Administration in Boulder, Colo., who was not involved in the research.

For starters, storms that pass over populated areas are more apt to be analyzed. “There’s historically been a pretty big population bias,” Kingfield says. Storms that occur over vegetated regions also tend to be well studied, simply because they leave obvious scars on the landscape. Ripped-up grasses or downed trees function like beacons to indicate the path of a storm, says Kingfield, who has studied forests damaged by tornadoes.

Spring and summer are peak storm seasons in the United States — more than 70 percent of tornadoes strike from March through September, according to NOAA. But on December 10, 2021, a cluster of storms started racing across the central and southern United States. Those tornadoes, which claimed more than 80 lives, swept across cities and also farmland, much of which had already been harvested for the season.

Jingyu Wang, a physical geographer at Nanyang Technological University in Singapore, and his colleagues set out to detect the signatures of those deadly storms in unpopulated, barren landscapes.

Swirling winds, even relatively weak ones, can suction up several centimeters of soil. And since deeper layers of the ground tend to be wetter, a tornado ought to leave behind a telltale signature: a long swath of moister-than-usual soil. Two properties linked with soil moisture level — its texture and temperature — in turn impact how much near-infrared light the soil reflects.

Wang and his collaborators analyzed near-infrared data collected by NASA’s Terra and Aqua satellites and looked for changes in soil moisture consistent with a passing tornado.

When the team looked at data obtained shortly after the 2021 storm outbreak, they noticed a signal in northeastern Arkansas. The feature was consistent with a roughly 60-kilometer-long track of wet soil. Tornadoes had been previously reported in that area — outside the city of Osceola — so it’s likely that this feature was created by a powerful storm, the team concluded.

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That makes sense, Kingfield says, and observations like these can reveal tornado signatures that might otherwise be missed. However, it’s important to acknowledge that this new technique works best in places where soils are capable of retaining water, he says. “You need to have clay-rich soils.”

Even so, these results hold promise for analyzing other tornadoes, Kingfield says. It’s always useful to have a new tool for estimating the strength, path and structure of a storm, but many storms go relatively unexamined simply because of where and when they occur, he says. “Now we have this new ground truth.” More

The 19th century landscape paintings hanging in London’s Tate Britain museum looked awfully familiar to climate physicist Anna Lea Albright. Artist Joseph Mallord William Turner’s signature way of shrouding his vistas in fog and smoke reminded Albright of her own research tracking air pollution.“I started wondering if there was a connection,” says Albright, who had been visiting the museum on a day off from the Laboratory for Dynamical Meteorology in Paris. After all, Turner — a forerunner of the impressionist movement — was painting as Britain’s industrial revolution gathered steam, and a growing number of belching manufacturing plants earned London the nickname “The Big Smoke.”

Turner’s early works, such as his 1814 painting “Apullia in Search of Appullus,” were rendered in sharp details. Later works, like his celebrated 1844 painting “Rain, Steam and Speed — the Great Western Railway,” embraced a dreamier, fuzzier aesthetic.

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Perhaps, Albright thought, this burgeoning painting style wasn’t a purely artistic phenomenon. Perhaps Turner and his successors painted exactly what they saw: their environs becoming more and more obscured by smokestack haze.

To find out how much realism there is in impressionism, Albright teamed up with Harvard University climatologist Peter Huybers, who’s an expert in reconstructing pollution before instruments existed to closely track air quality. Their analysis of nearly 130 paintings by Turner, Paris-based impressionist Claude Monet and several others tells a tale of two modernizing cities.

Low contrast and whiter hues are hallmarks of the impressionist style. They are also hallmarks of air pollution, which can affect how a distant scene looks to the naked eye. Tiny airborne particles, or aerosols, can absorb or scatter light. That makes the bright parts of objects appear dimmer while also shifting the entire scene’s color toward neutral white.

The artworks that Albright and Huybers investigated, which span from the late 1700s to the early 1900s, decrease in contrast as the 19th century progresses. That trend tracks with an increase in air pollution, estimated from historical records of coal sales, Albright and Huybers report in the Feb. 7 Proceedings of the National Academy of Sciences.

“Our results indicate that [19th century] paintings capture changes in the optical environment associated with increasingly polluted atmospheres during the industrial revolution,” the researchers write.

Albright and Huybers distinguished art from aerosol by first using a mathematical model to analyze the contrast and color of 60 paintings that Turner made between 1796 and 1850 as well as 38 Monet works from 1864 to 1901. They then compared the findings to sulfur dioxide emissions over the century, estimated from the trend in the annual amount of coal sold and burned in London and Paris. When sulfur dioxide reacts with molecules in the atmosphere, aerosols form.

The early works of British painter Joseph Mallord William Turner, such as “Apullia in Search of Appullus,” left, painted in 1814, were rendered in sharp details. His later works, like “Rain, Steam and Speed — the Great Western Railway,” right, painted in 1844, embraced a dreamier aesthetic. The decrease in contrast between the paintings tracks with increasing air pollution from the industrial revolution, researchers say.From left: Apullia in Search of Appullus vide Ovid, Joseph Mallord William Turner/The Tate Collection (CC BY-NC-ND 3.0); World History Archive/Alamy Stock Photo

As sulfur dioxide emissions increased over time, the amount of contrast in both Turner’s and Monet’s paintings decreased. However, paintings of Paris that Monet made from 1864 to 1872 have much higher contrast than Turner’s last paintings of London made two decades earlier.

The difference, Albright and Huybers say, can be attributed to the much slower start of the industrial revolution in France. Paris’ air pollution level around 1870 was about what London’s was when Turner started painting in the early 1800s. It confirms that the similar progression in their painting styles can’t be chalked up to coincidence, but is guided by air pollution, the pair conclude.

The researchers also analyzed the paintings’ visibility, or the distance at which an object can be clearly seen. Before 1830, the visibility in Turner’s paintings averaged about 25 kilometers, the team found. Paintings made after 1830 had an average visibility of about 10 kilometers. Paintings made by Monet in London around 1900, such as “Charing Cross Bridge,” have a visibility of less than five kilometers. That’s similar to estimates for modern-day megacities such as Delhi and Beijing, Albright and Huybers say.

To strengthen their argument, the researchers also analyzed 18 paintings from four other London- and Paris-based impressionists. Again, as outdoor air pollution increased over time, the contrast and visibility in the paintings decreased, the team found. What’s more, the decrease seen in French paintings lagged behind the decrease seen in British ones.

Overall, air pollution can explain about 61 percent of contrast differences between the paintings, the researchers calculate. In that respect, “different painters will paint in a similar way when the environment is similar,” Albright says. “But I don’t want to overstep and say: Oh, we can explain all of impressionism.” More