A steady stratified purely azimuthal flow representing the Antarctic Circumpolar Current

Abstract We construct an explicit steady stratified purely azimuthal flow for the governing equations of geophysical fluid dynamics. These equations are considered in a setting that applies to the Antarctic Circumpolar Current, accounting for eddy viscosity and forcing terms.

Bibliographic Details
Published in:Monatshefte für Mathematik
Main Authors: Martin, Calin Iulian, Quirchmayr, Ronald
Other Authors: Austrian Science Fund
Format: Article in Journal/Newspaper
Language:English
Published: Springer Science and Business Media LLC 2019
Subjects:
General Mathematics
Antarctic
The Antarctic
Antarc*
Online Access:http://dx.doi.org/10.1007/s00605-019-01332-3
http://link.springer.com/content/pdf/10.1007/s00605-019-01332-3.pdf
http://link.springer.com/article/10.1007/s00605-019-01332-3/fulltext.html
Description
Summary:Abstract We construct an explicit steady stratified purely azimuthal flow for the governing equations of geophysical fluid dynamics. These equations are considered in a setting that applies to the Antarctic Circumpolar Current, accounting for eddy viscosity and forcing terms.

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