Internal dissipative boundary layers in the cross-equatorial flow of a grounded deep western boundary current
Author:
Affiliation:
1. Department of Mathematical and Statistical Sciences, Applied Mathematics Institute, University of Alberta, Edmonton, Canada.
2. Institute for Geophysical Research, University of Alberta, Edmonton, Canada.
Funder
Natural Sciences and Engineering Research Council of Canada
Natural Sciences and Engineering Research Council (NSERC) of Canada
Publisher
Informa UK Limited
Subject
Geochemistry and Petrology,Mechanics of Materials,Geophysics,Astronomy and Astrophysics,Computational Mechanics
Link
https://www.tandfonline.com/doi/pdf/10.1080/03091929.2017.1287909
Reference27 articles.
1. Observed and simulated estimates of the meridional overturning circulation at 26.5° N in the Atlantic
2. Deep, cross-equatorial eddies
3. Shallow water modeling of Antarctic Bottom Water crossing the equator
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1. The Parametrization of the Cauchy Problem for Nonlinear Differential Equations with Contrast Structures;Mordovia University Bulletin;2018-12-28
2. Hamiltonian Structure and a Variational Principle for Grounded Abyssal Flow on a Sloping Bottom in a Mid-Latitude β-Plane;Studies in Applied Mathematics;2018-07-05
3. Meridional dynamics of grounded abyssal water masses on a sloping bottom in a mid-latitude -plane;Journal of Fluid Mechanics;2018-02-26
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