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Climate models disagree on the sign of total radiative feedback in the Arctic

Climate feedbacks have been found to strongly impact the observed amplified Arctic warming. However, Arctic amplification is modeled with a wide spread which partly arises from intermodel differences of the various feedbacks. To explain the spread in modeled Arctic warming, feedback uncertainties an...

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Detaylı Bibliyografya
Asıl Yazarlar: Karoline Block, Florian A. Schneider, Johannes Mülmenstädt, Marc Salzmann, Johannes Quaas
Materyal Türü: Artigo
Dil:Inglês
Baskı/Yayın Bilgisi: Stockholm University Press 2020-01-01
Seri Bilgileri:Tellus: Series A, Dynamic Meteorology and Oceanography
Konular:
Online Erişim:http://dx.doi.org/10.1080/16000870.2019.1696139
Etiketler: Etiketle
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