Reductions in midlatitude upwelling-favorable winds implied by weaker large-scale Pliocene SST gradients
Author:
Affiliation:
1. Department of Earth and Planetary Sciences; Harvard University; Cambridge Massachusetts USA
2. School of Engineering and Applied Science; Harvard University; Cambridge Massachusetts USA
Funder
NSF Graduate Research Fellowship (NPA)
NSF Climate Dynamics
Publisher
American Geophysical Union (AGU)
Subject
Paleontology,Oceanography
Reference62 articles.
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2. The seasonal cycle of wind-stress curl in subtropical eastern boundary current regions;Bakun;J. Phys. Ocean.,1991
3. Response of the tropical Pacific to changes in extratropical clouds;Barreiro;Clim. Dyn.,2008
4. The thermal structure of the upper ocean;Boccaletti;J. Phys. Ocean.,2004
5. What shapes mesoscale wind anomalies in coastal upwelling zones?;Boé;Clim. Dyn.,2011
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