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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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| I publikationen: | Sci Rep |
|---|---|
| Huvudupphovsmän: | , , , , |
| Materialtyp: | Artigo |
| Språk: | Inglês |
| Publicerad: |
Nature Publishing Group UK
2017
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| Ämnen: | |
| Länkar: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5684145/ https://ncbi.nlm.nih.gov/pubmed/29133905 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41598-017-15637-6 |
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