As air temperatures rise, North Slope soils as deep as 20 meters below the surface are warming at a rate of up to 4 degrees Celsius per decade, according to long-term measurements by UAF scientists. (via AlaskaBeacon)
by Williams College researchers presented in mid-December at the annual conference of the American Geophysical Union.
There are more subtle factors, too, which Ravens listed at a permafrost workshop held in Anchorage in November. A change in precipitation patterns from snow to rain sends heat from the surface into the soil. The ocean water, aside from bringing soils in contact with heat, also contains salt, another thaw factor. Long-term thawing is causing vast stretches of land to sink, pulling down the coastline along with the rest of the landscape.
The U.S. Army Corps of Engineers is putting the final touches on the design for five miles of what’s known as a “” to protect the shoreline. It is a massive project that has been several years in the planning and is expected to take at least six years to complete, said Bruce Sexauer, chief of civil works project management for the Corps of Engineers’ Alaska district.
“If Utqiagvik suddenly had a catastrophic issue, that would have an effect on the other communities in the area,” Sexauer said. That danger materialized in a different North Slope community in the spring of 2021. In Point Lay, 180 miles southwest of Utqiagvik, a sudden thaw collapse in the permafrost, temporarily cutting off flow of water to the village clinic and to several houses. It was a particularly ill-timed event, as it came during the COVID-19 pandemic, when clean water became a critical need.
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