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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Bibliographische Detailangaben
Veröffentlicht in:Monatshefte für Mathematik 2020, Vol.192 (2), p.401-407
Hauptverfasser: Martin, Calin Iulian, Quirchmayr, Ronald
Format: Artikel
Sprache:eng
Schlagworte:
Antarctic Circumpolar Current
Azimuthal flows
Eddy currents
Eddy viscosity
Fluid dynamics
Geophysical fluid dynamics
Geophysical fluids
Mathematical analysis
Mathematics
Mathematics and Statistics
Physical Sciences
Science & Technology
Variable density
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:0026-9255
1436-5081
1436-5081
DOI:10.1007/s00605-019-01332-3