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Magnitude and pattern of Arctic warming governed by the seasonality of radiative forcing
Observed and projected climate warming is strongest in the Arctic regions, peaking in autumn/winter. Attempts to explain this feature have focused primarily on identifying the associated climate feedbacks, particularly the ice-albedo and lapse-rate feedbacks. Here we use a state-of-the-art global cl...
| Autores principales: | , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
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Nature Publishing Group
2016
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| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5133621/ https://www.ncbi.nlm.nih.gov/pubmed/27910905 http://dx.doi.org/10.1038/srep38287 |