
Thermokarst lakes, formed by thawing permafrost, in Alaska
Asahi Shimbun via Getty Images
As the Arctic warms, large amounts of greenhouse gases may be released from lake bottom sediment, a previously overlooked source.
Frozen ground in the Arctic has already begun to thaw, releasing more methane and carbon dioxide into the atmosphere. This climate feedback is knownbut most modeling only accounts for thawing in the top 3 meters of Arctic soil.
Deep…