Indian monsoon variability during the last 46kyr: isotopic records of planktic foraminifera from southwestern Bay of Bengal

The Indian monsoon carries large amounts of freshwater to the northern Indian Ocean and modulates the upper ocean structure in terms of upwelling and productivity. Freshwater‐induced stratification in the upper ocean of the Bay of Bengal is linked to the changes in the Indian monsoon. In this study,...

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Veröffentlicht in:	Journal of quaternary science 2021-01, Vol.36 (1), p.138-151
Hauptverfasser:	Gautam, P K, Narayana, A C, Kumar, P Kiran, Bhavani, P G, Yadava, M G, Jull, A J T
Format:	Artikel
Sprache:	eng
Schlagworte:	Atmospheric variability Foraminifera Last Glacial Maximum Monsoons Oceans Rain Upper ocean Upwelling Variability Wind
Online-Zugang:	Volltext
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