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Winter amplification of the European Little Ice Age cooling by the subpolar gyre
Climate reconstructions reveal a strong winter amplification of the cooling over central and northern continental Europe during the Little Ice Age period (LIA, here defined as c. 16th–18th centuries) via persistent, blocked atmospheric conditions. Although various potential drivers have been suggest...
Uloženo v:
| Vydáno v: | Sci Rep |
|---|---|
| Hlavní autoři: | , , , , |
| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
Nature Publishing Group UK
2017
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| Témata: | |
| On-line přístup: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5577174/ https://ncbi.nlm.nih.gov/pubmed/28855516 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41598-017-07969-0 |
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