Role of Residual Overturning for the Sensitivity of Southern Ocean Isopycnal Slopes to Changes in Wind Forcing
Author:
Affiliation:
1. MIT–WHOI Joint Program in Oceanography, Cambridge, Massachusetts
2. Department of Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, Massachusetts
Abstract
Funder
Directorate for Geosciences
Division of Atmospheric and Geospace Sciences
Division of Ocean Sciences
National Defense Science and Engineering Graduate
Publisher
American Meteorological Society
Subject
Oceanography
Link
http://journals.ametsoc.org/jpo/article-pdf/49/11/2867/4851411/jpo-d-19-0072_1.pdf
Reference45 articles.
1. Topographic enhancement of eddy efficiency in baroclinic equilibration;Abernathey;J. Phys. Oceanogr.,2014
2. Jet–topography interactions affect energy pathways to the deep Southern Ocean;Barthel;J. Phys. Oceanogr.,2017
3. Southern Ocean overturning compensation in an eddy-resolving climate simulation;Bishop;J. Phys. Oceanogr.,2016
4. Geographical variability of the first baroclinic Rossby radius of deformation;Chelton;J. Phys. Oceanogr.,1998
5. A barotropic model of eddy saturation;Constantinou;J. Phys. Oceanogr.,2018
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