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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Bibliographic Details
Published inNPJ climate and atmospheric science Vol. 3; no. 1
Main Authors Feldl, Nicole, Po-Chedley, Stephen, Singh, Hansi K. A., Hay, Stephanie, Kushner, Paul J.
Format Journal Article
LanguageEnglish
Published London Nature Publishing Group UK 22.10.2020
Nature Publishing Group
Springer Nature
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