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...
| Main Authors: | , , , , |
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| 格式: | 文件 |
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Nature Publishing Group
2017
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| 在线阅读: | http://hdl.handle.net/1721.1/112628 |