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...

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Detalles Bibliográficos
Autores principales: Moreno-Chamarro, Eduardo, Zanchettin, Davide, Lohmann, Katja, Luterbacher, Jürg, Jungclaus, Johann H.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2017
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5577174/
https://www.ncbi.nlm.nih.gov/pubmed/28855516
http://dx.doi.org/10.1038/s41598-017-07969-0

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5577174/
https://www.ncbi.nlm.nih.gov/pubmed/28855516
http://dx.doi.org/10.1038/s41598-017-07969-0

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