Rapid sea-ice loss may increase the rate of Arctic land warming by 3.5 times – affecting permafrost
Recently a mysterious Siberian crater has been discovered, which subsequently […]
July 25, 2014
Recently a mysterious Siberian crater has been discovered, which subsequently raised questions about the circumstances surrounding the crater formation. Theories include Pingo formation and connections to the thawing of permafrost (ClimateState reported).
Robert Scribbler, summed it up: One theory on the feature is that it might be a pingo — a melting of a permafrost water pocket left over by an ancient lake that was long ago buried by sediment. But a pingo would typically form in a manner similar to a sinkhole and would probably not have apparent ejected material piled around its mouth.
Another theory, advanced by Russian Arctic scientists, is that a pocket of gas beneath the permafrost spontaneously destabilized — either through chemical or physical processes. The destabilized gas then is thought to have violently blown away the surface layer “like the popping of a cork in a champagne bottle.”
“Our study suggests that, if sea-ice continues to contract rapidly over the next several years, Arctic land warming and permafrost thaw are likely to accelerate.”
NCAR’s press release explained:
The team found that during episodes of rapid sea-ice loss, the rate of Arctic land warming is 3.5 times greater than the average 21st century warming rates predicted in global climate models. While this warming is largest over the ocean, the simulations suggest that it can penetrate as far as 900 miles inland. The simulations also indicate that the warming acceleration during such events is especially pronounced in autumn. The decade during which a rapid sea-ice loss event occurs could see autumn temperatures warm by as much as 9 degrees F (5 degrees C) along the Arctic coasts of Russia, Alaska, and Canada.
Lawrence and his colleagues then used the model to study the influence of accelerated warming on permafrost and found that in areas where permafrost is already at risk, such as central Alaska, a period of abrupt sea-ice loss could lead to rapid soil thaw. This situation, when summer thaw extends more deeply than the next winter’s freeze, can lead to a talik, which is a layer of permanently unfrozen soil sandwiched between the seasonally frozen layer above and the perennially frozen layer below. A talik allows heat to build more quickly in the soil, hastening the long-term thaw of permafrost.
Recent warming has degraded large sections of permafrost, with pockets of soil collapsing as the ice within it melts. The results include buckled highways, destabilized houses, and “drunken forests” of trees that lean at wild angles.
“An important unresolved question is how the delicate balance of life in the Arctic will respond to such a rapid warming,” Lawrence says. “Will we see, for example, accelerated coastal erosion, or increased methane emissions, or faster shrub encroachment into tundra regions if sea ice continues to retreat rapidly?”
It appears that craters may be added to the list of visible signs of permafrost degradation.
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