Equatorial Pacific forcing of western Amazonian precipitation during Heinrich Stadial 1

Abundant hydroclimatic evidence from western Amazonia and the adjacent Andes documents wet conditions during Heinrich Stadial 1 (HS1, 18–15 ka), a cold period in the high latitudes of the North Atlantic. This precipitation anomaly was attributed to a strengthening of the South American summer monsoo...

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Detalles Bibliográficos
Autores principales: Zhang, Yancheng, Zhang, Xu, Chiessi, Cristiano M., Mulitza, Stefan, Zhang, Xiao, Lohmann, Gerrit, Prange, Matthias, Behling, Hermann, Zabel, Matthias, Govin, Aline, Sawakuchi, André O., Cruz, Francisco W., Wefer, Gerold
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2016
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5078807/
https://www.ncbi.nlm.nih.gov/pubmed/27779213
http://dx.doi.org/10.1038/srep35866

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5078807/
https://www.ncbi.nlm.nih.gov/pubmed/27779213
http://dx.doi.org/10.1038/srep35866

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