In Alaska, soil in permafrost regions is warming the fastest

New research from Washington State University indicates that soil in Alaska is warming rapidly, particularly in permafrost regions. This trend threatens infrastructure stability and risks accelerating climate change through the release of trapped carbon dioxide and methane.
Why it matters
Understanding the rate of permafrost thaw is critical for predicting global climate feedback loops and managing infrastructure in Arctic regions.
by Shawn Vestal, Washington State University
edited by Sadie Harley , reviewed by Robert Egan
This article has been reviewed according to Science X's editorial process and policies . Editors have highlighted the following attributes while ensuring the content's credibility:
Add as preferred source Credit: CC0 Public Domain Soils are warming quickly and at considerable depth across Alaska, with temperatures rising fastest in the state's permafrost region, a trend that could accelerate climate change and undermine the stability of roads, buildings and other infrastructure built on the continuously frozen ground.
That's a central finding of new research from Washington State University that provides a comprehensive look at soil temperatures from 1997 to 2023 in a state where the effects of climate change are pronounced. The warming permafrost is of particular concern because when that ground thaws, it releases carbon dioxide and methane, driving even faster warming.
Get smarter about the news
Sign up free for a feed built around what you actually care about, Dive Deeper research on any story, and the full text of every article.
Create free accountAlready have an account? Sign in