Deglacial Tropical Atlantic subsurface warming links ocean circulation variability to the West African Monsoon

Multiple lines of evidence show that cold stadials in the North Atlantic were accompanied by both reductions in Atlantic Meridional Overturning Circulation (AMOC) and collapses of the West African Monsoon (WAM). Although records of terrestrial change identify abrupt WAM variability across the deglac...

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Detalles Bibliográficos
Autores principales: Schmidt, Matthew W., Chang, Ping, Parker, Andrew O., Ji, Link, He, Feng
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/PMC5684145/
https://www.ncbi.nlm.nih.gov/pubmed/29133905
http://dx.doi.org/10.1038/s41598-017-15637-6

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5684145/
https://www.ncbi.nlm.nih.gov/pubmed/29133905
http://dx.doi.org/10.1038/s41598-017-15637-6

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