Sea ice and atmospheric circulation shape the high-latitude lapse rate feedback
Arctic amplification of anthropogenic climate change is widely attributed to the sea-ice albedo feedback, with its attendant increase in absorbed solar radiation, and to the effect of the vertical structure of atmospheric warming on Earth’s outgoing longwave radiation. The latter lapse rate feedback...
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Published in | NPJ climate and atmospheric science Vol. 3; no. 1 |
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Main Authors | , , , , |
Format | Journal Article |
Language | English |
Published |
London
Nature Publishing Group UK
22.10.2020
Nature Publishing Group Springer Nature |
Subjects | |
Online Access | Get full text |
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