A steady stratified purely azimuthal flow representing the Antarctic Circumpolar Current

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.

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Veröffentlicht in:arXiv.org 2020-10
Hauptverfasser: Calin Iulian Martin, Quirchmayr, Ronald
Format: Artikel
Sprache:eng
Schlagworte:
Eddy currents
Eddy viscosity
Fluid dynamics
Geophysical fluids
Mathematical analysis
Mathematics - Analysis of PDEs
Physics - Atmospheric and Oceanic Physics
Physics - Fluid Dynamics
Viscosity
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Beschreibung
Zusammenfassung: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.
ISSN:2331-8422
DOI:10.48550/arxiv.2010.09389