A steady stratified purely azimuthal flow representing the Antarctic Circumpolar Current

Calin Iulian Martin; Ronald Quirchmayr

doi:10.1007/s00605-019-01332

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arXiv · 2010.09389

A steady stratified purely azimuthal flow representing the Antarctic Circumpolar Current

Calin Iulian Martin·Ronald Quirchmayr

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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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Calin Iulian Martin, Ronald Quirchmayr. 2020-10-19. A steady stratified purely azimuthal flow representing the Antarctic Circumpolar Current. https://doi.org/10.1007/s00605-019-01332

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