Contribution of Atmospheric Advection to the Amplified Winter Warming in the Arctic North Atlantic Region

Arctic Amplification of climate warming is caused by various feedback processes in the atmosphere-ocean-ice system and yields the strongest temperature increase during winter in the Arctic North Atlantic region. In our study, we attempt to quantify the advective contribution to the observed atmosphe...

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Bibliographic Details
Main Authors: Sandro Dahlke, Marion Maturilli
Format: Article
Language:English
Published: Wiley 2017-01-01
Series:Advances in Meteorology
Online Access:http://dx.doi.org/10.1155/2017/4928620
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