Arctic summer sea ice is receding faster than previously projected and is expected to virtually disappear before 2050. We have seen dramatic decreases since the late 1970s, particularly in summer and autumn.
Ice loss increases Arctic warming by replacing white, reflective ice with dark water that absorbs more energy from the sun, creating a “feedback cycle” that results in more ice loss.
The Alaska Center for Climate Assessment and Policy publishes regularly updated sea ice graphics that give updates on seasonally relevant ice extent and ice thickness, plus historical analyses.
Ice impacts everything
Less ice can increase access for ships—and the potential for marine accidents in remote regions where help is usually very far away.
Shorelines are less protected from storms and more likely to erode.
Less ice means less food: the underside of sea ice supports large colonies of algae. When the ice melts in the spring, algae falls into the water column, providing nutrients that feed plankton, which in turn supports fish, seals, whales and walruses.
Permafrost lies beneath 80% of Alaska. It contains vast quantities of carbon that can be emitted as carbon dioxide and methane, powerful greenhouse gases.
When permafrost thaws, it slumps, causes subsidence, slope instability, and erosion. This can impact buildings, roads, water quality, wildlife, and food security.
Work by UAF permafrost researcher Vladimir Romanovsky suggests that if warming keeps progressing, more than half of the permafrost of Alaska's North Slope—a region bigger than Minnesota—could thaw by century’s end.