Arctic lakes are drying up, according to a new study.
The finding flashes a new warning light on the global climate dashboard.
The Arctic is no stranger to loss. As the region warms nearly four times faster than the rest of the world, glaciers collapse, wildlife suffers, and habitats continue to disappear at a record pace.
“…permafrost thaw is occurring even faster than we as a community had anticipated.”
The new research reveals that over the past 20 years, Arctic lakes have shrunk or dried completely across the pan-Arctic, a region spanning the northern parts of Canada, Russia, Greenland, Scandinavia, and Alaska.
The findings offer clues about why the mass drying is happening and how the loss can be slowed.
Surprising arctic lake decline
The vanishing lakes act as cornerstones of the Arctic ecosystem. They provide a critical source of fresh water for local Indigenous communities and industries. Threatened and endangered species, including migratory birds and aquatic creatures, also rely on the lake habitats for survival.
The lake decline comes as a surprise. Scientists had predicted that climate change would initially expand lakes across the tundra, due to land surface changes resulting from melting ground ice, with eventual drying in the mid-21st or 22nd century.
Instead, it appears that thawing permafrost, the frozen soil that blankets the Arctic, may drain lakes and outweigh this expansion effect, says Elizabeth Webb, a postdoctoral researcher in the biology department at the University of Florida, and lead author of the study in Nature Climate Change.
Webb and colleagues theorized that thawing permafrost may decrease lake area by creating drainage channels and increasing soil erosion into the lakes.
“Our findings suggest that permafrost thaw is occurring even faster than we as a community had anticipated,” Webb says. “It also indicates that the region is likely on a trajectory toward more landscape-scale drainage in the future.”
Counterintuitive finding
In addition to rising temperatures, the study also reveals that increases in autumn rainfall cause permafrost degradation and lake drainage.
“It might seem counterintuitive that increasing rainfall reduces surface water,” says Jeremy Lichstein, Webb’s advisor and a study coauthor. “But it turns out the physical explanation was already in the scientific literature: rainwater carries heat into the soil and accelerates permafrost thaw, which can open up underground channels that drain the surface.”
If accelerated permafrost thaw is to blame, that’s unwelcome news. The Arctic permafrost is a natural warehouse of preserved organic matter and planet-warming gases.
“Permafrost soils store nearly two times as much carbon as the atmosphere,” Webb says. “There’s a lot of ongoing research suggesting that as permafrost thaws, this carbon is vulnerable to being released to the atmosphere in the form of methane and carbon dioxide.”
‘The snowball is already rolling’
There is a silver lining in the findings. Previous models of lake dynamics predicted lake expansion, which thaws the surrounding permafrost. But because lakes are drying, permafrost near the lakes is likely not thawing as fast.
“It’s not immediately clear exactly what the trade-offs are, but we do know that lake expansion causes carbon losses orders of magnitude higher than occurs in surrounding regions,” Webb says.
To achieve their results, Webb’s team used satellite data to identify broad trends in surface water change across the Arctic. Known as remote sensing, satellite imagery helps answer broad-scale questions, says Webb.
“One of the things that I really like about using remote sensing is that you can answer what seemed like impossibly big questions—we have the ability to answer them now,” Webb says. “It’s only in the past five, 10 years that we’ve had the computing power and resources to pull this off.”
The research team used a machine-learning approach to examine the climate change mechanisms responsible for lake area change. By harnessing large ensembles of satellite images to assess patterns of surface water loss, they were able to analyze decades of data across the Arctic.
Their work relied on robust programs, including Google Earth Engine and the Python platform on the University of Florida’s HiPerGator supercomputer, to query large data sets and run models.
Webb initially set out to explore a different topic altogether: Arctic albedo, or surface reflectivity. Webb’s earlier work showed that surface water is an important driver of albedo change, but she struggled to locate studies that detailed why the surface waters were changing in the first place. “I wrote the paper I wanted to cite for my albedo work,” she says.
To curtail the lakes’ demise, recent research shows that perhaps the best way to save permafrost is by cutting fossil fuel emissions. Reducing carbon emissions could put the planet back on track by limiting global temperature rise.
“The snowball is already rolling,” Webb says, stating that we need to act now to slow these changes. “It’s not going to work to keep on doing what we’re doing.”
The University of Florida’s School of Natural Resources and Environment and a NASA FINESST fellowship funded Webb’s work. Additional coauthors are from the University of Florida, the Woodwell Climate Research Center, Colgate University, and the University of Connecticut.
Source: Lauren Barnett for University of Florida
