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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...

Ausführliche Beschreibung

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Bibliographische Detailangaben
Hauptverfasser: Karoline Block, Florian A. Schneider, Johannes Mülmenstädt, Marc Salzmann, Johannes Quaas
Format: Artigo
Sprache:Inglês
Veröffentlicht: Stockholm University Press 2020-01-01
Schriftenreihe:Tellus: Series A, Dynamic Meteorology and Oceanography
Schlagworte:
Online Zugang:http://dx.doi.org/10.1080/16000870.2019.1696139
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