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Underlying causes of Eurasian midcontinental aridity in simulations of mid‐Holocene climate
Climate model simulations uniformly show drier and warmer summers in the Eurasian midcontinent during the mid‐Holocene, which is not consistent with paleoenvironmental observations. The simulated climate results from a reduction in the zonal temperature gradient, which weakens westerly flow and redu...
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| Publicado no: | Geophys Res Lett |
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| Main Authors: | , , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
John Wiley and Sons Inc.
2017
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| Assuntos: | |
| Acesso em linha: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5661745/ https://ncbi.nlm.nih.gov/pubmed/29104328 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1002/2017GL074476 |
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