טוען...
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...
שמור ב:
| הוצא לאור ב: | Sci Rep |
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| Main Authors: | , , , , , , , , , , , , |
| פורמט: | Artigo |
| שפה: | Inglês |
| יצא לאור: |
Nature Publishing Group
2016
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| נושאים: | |
| גישה מקוונת: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5078807/ https://ncbi.nlm.nih.gov/pubmed/27779213 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/srep35866 |
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