Enhancement in vertical fluxes at a front by mesoscale-submesoscale coupling-Reference-Cited by-同舟云学术

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Enhancement in vertical fluxes at a front by mesoscale-submesoscale coupling

Published:2014-12 Issue:12 Volume:119 Page:8495-8511
ISSN:2169-9275
Container-title:Journal of Geophysical Research: Oceans
language:en
Short-container-title:J. Geophys. Res. Oceans

Author:

Ramachandran Sanjiv¹,Tandon Amit¹²,Mahadevan Amala³

Affiliation:

1. Department of Mechanical Engineering; University of Massachusetts; Dartmouth Massachusetts USA

2. School of Marine Sciences, University of Massachusetts; Dartmouth Massachusetts USA

3. Woods Hole Oceanographic Institution; Woods Hole Massachusetts USA

Funder

National Science Foundation

Office of Naval Research

Publisher

American Geophysical Union (AGU)

Subject

Earth and Planetary Sciences (miscellaneous),Space and Planetary Science,Geochemistry and Petrology,Geophysics,Oceanography

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1002/2014JC010211/fullpdf

Reference47 articles.

1. Baroclinic instability and submesoscale eddy formation in weakly stratified oceans under cooling;Akitomo;J. Geophys. Res.,2010

2. Planetary waves in horizontal and vertical shear: The generalized Eliasen-Palm relation and the mean zonal acceleration;Andrews;J. Atmos. Sci.,1976

3. Mixed layer instabilities and restratification;Boccaletti;J. Phys. Oceanogr.,2007

4. Mesoscale to submesoscale transition in the California Current System. Part I: Flow structure, eddy flux and observational tests;Capet;J. Phys. Oceanogr.,2008a

5. Mesoscale to submesoscale transition in the California Current System. Part II: Frontal processes;Capet;J. Phys. Oceanogr.,2008b

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