A new study suggests the Arctic's cap of cold, layered air plays a more important role in boosting polar warming than does its shrinking ice and snow cover. A layer of shallow, stagnant air acts like a lid, concentrating heat near the surface, researchers reported last Sunday (Feb. 2) in the journal Nature Geoscience.
"In the Arctic, as the climate warms, most of the additional heat remains trapped in a shallow layer of the atmosphere close to the ground, not deeper than 1 or 2 kilometers [0.6 to 1.2 miles]," said Felix Pithan, a climate scientist at the Max Planck Institute for Meteorology in Germany and lead author of the new study.
"[This] makes the Arctic surface rather inefficient at getting rid of extra energy, and therefore it warms more than other regions when the entire planet is warming," Pithan told Live Science.
Arctic's 'Layer Cake' Atmosphere Blamed for Rapid Warming
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