A steady stratified purely azimuthal flow representing the Antarctic Circumpolar Current

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
Main Authors: Martin, Calin Iulian, Quirchmayr, Ronald
Format: Article in Journal/Newspaper
Language:unknown
Published: arXiv 2020
Subjects:
Fluid Dynamics physics.flu-dyn
Analysis of PDEs math.AP
Atmospheric and Oceanic Physics physics.ao-ph
FOS Physical sciences
FOS Mathematics
Antarctic
The Antarctic
Antarc*
Online Access:https://dx.doi.org/10.48550/arxiv.2010.09389
https://arxiv.org/abs/2010.09389
Description
Summary: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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