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Alaskan land eroding faster due to climate change

Alaskan land eroding faster due to climate change
Field photos of the Koyukuk River, Alaska. (a) Map of Alaska with the Yukon River system shown in light blue and the Koyukuk River in dark blue. (b) Aerial image showing scroll bar complexes outlined by vegetation across the Koyukuk River floodplain near Huslia, Alaska. Boat for scale (white circle) is the same boat depicted in (d). (c) Seasonally frozen bank with large white spruce and willow trees tipping into the river as the bank erodes. (d) Cutbank containing permafrost and ice wedges overlain by a thick layer of peat and mosses with few trees. Credit: AGU Advances (2024). DOI: 10.1029/2024AV001175

A new study out of The University of Texas at Arlington shows that frozen land in Alaska is eroding faster than it can be replaced due to climate change.

"In the Northern Hemisphere, much of the ground is , meaning it is frozen year-round. Permafrost is a delicate natural resource. If it is lost faster than it is regenerated, we endanger infrastructure and release , which can warm the atmosphere," said Nathan D. Brown, assistant professor of earth and environmental sciences at UT Arlington.

"Under a , a major question is whether will erode permafrost in thawing riverbanks faster than permafrost can regenerate."

It happens slowly, but all rivers naturally change their paths over time. Floods, earthquakes, , and wildlife are constantly at work shifting rivers, charting new paths for water, and depositing sediment where water once flowed.

A difference seen with Alaskan rivers is that the land on riverbanks can be permanently frozen. Called permafrost, it's a mixture of soil, gravel and sand often bound together by ice. Permafrost is important because it holds large amounts of organic carbon, which is then released when it melts. This carbon can combine with oxygen to become , a greenhouse gas that warms Earth's atmosphere.

To better understand the fate of permafrost in a warming world, Dr. Brown—along with colleagues from the California Institute of Technology; Massachusetts Institute of Technology; University of California at Santa Barbara; Los Alamos National Laboratory; the University of Chicago; and the University of Pennsylvania—mapped and dated floodplain deposits, determined permafrost extent, and characterized vegetation along the Koyukuk River in Alaska to model how permafrost formation varies with air temperature.

The Koyukuk is a 425-mile feeder stream of the Yukon River and the last major tributary to flow into the Yukon before it empties into the Bering Sea, the major waterway separating America and Russia.

In the journal AGU Advances, the team reported that while new permafrost is developing along the Koyukuk River floodplain, it is not forming fast enough to replace what is disappearing due to rising temperatures.

"By dating these permafrost deposits, we found that permafrost formation in this region can take thousands of years," said Brown. "Under a warming climate, permafrost formation is expected to take longer, while thawing permafrost riverbanks will become more susceptible to erosion. The net result will be loss of permafrost and contribution of carbon to the atmosphere."

More information: Madison M. Douglas et al, Permafrost Formation in a Meandering River Floodplain, AGU Advances (2024). DOI: 10.1029/2024AV001175

Journal information: AGU Advances

Citation: Alaskan land eroding faster due to climate change (2024, August 7) retrieved 7 August 2024 from https://phys.org/news/2024-08-alaskan-eroding-faster-due-climate.html
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