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: | Zanchettin, Davide, Lohmann, Katja, Luterbacher, Jürg, Jungclaus, Johann H., Moreno Chamarro, Eduardo |
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Other Authors: | Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences |
Format: | Article |
Published: |
Nature Publishing Group
2017
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Online Access: | http://hdl.handle.net/1721.1/112628 |
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