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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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Detalles Bibliográficos
Main Authors: Karoline Block, Florian A. Schneider, Johannes Mülmenstädt, Marc Salzmann, Johannes Quaas
Formato: Artigo
Idioma:Inglês
Publicado: Stockholm University Press 2020-01-01
Series:Tellus: Series A, Dynamic Meteorology and Oceanography
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Acceso en liña:http://dx.doi.org/10.1080/16000870.2019.1696139
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