A steady stratified purely azimuthal flow representing the Antarctic Circumpolar Current.

Pub Date : 2020-01-01 Epub Date: 2019-09-12 DOI:10.1007/s00605-019-01332-3
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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代表南极环极洋流的稳定分层纯方位流。
我们为地球物理流体动力学的支配方程构建了一个明确的稳定分层纯方位流。这些方程是在适用于南极环极洋流的情况下考虑的,并考虑了涡流粘度和强迫项。
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