South Atlantic Surface Boundary Current System during the Last Millennium in the CESM-LME: The Medieval Climate Anomaly and Little Ice Age

South Atlantic Surface Boundary Current System during the Last Millennium in the CESM-LME: The Medieval Climate Anomaly and Little Ice Age

Interocean waters that are carried northward through South Atlantic surface boundary currents get meridionally split between two large-scale systems when meeting the South American coast at the western subtropical portion of the basin. This distribution of the zonal flow along the coast is investiga...

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Bibliographic Details
Main Authors: Fernanda Marcello, Ilana Wainer, Peter R. Gent, Bette L. Otto-Bliesner, Esther C. Brady
Format: Article
Language:English
Published: MDPI AG 2019-07-01
Series:Geosciences
Subjects:
equatorial current bifurcation
western boundary currents
South Atlantic Subtropical Gyre
Meridional Overturning Circulation
Last Millennium
Medieval Climate Anomaly
Little Ice Age
Online Access:https://www.mdpi.com/2076-3263/9/7/299

Internet

https://www.mdpi.com/2076-3263/9/7/299

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