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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...
Wedi'i Gadw mewn:
| Prif Awduron: | , , , , |
|---|---|
| Fformat: | Artigo |
| Iaith: | Inglês |
| Cyhoeddwyd: |
Stockholm University Press
2020-01-01
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| Cyfres: | Tellus: Series A, Dynamic Meteorology and Oceanography |
| Pynciau: | |
| Mynediad Ar-lein: | http://dx.doi.org/10.1080/16000870.2019.1696139 |
| Tagiau: |
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