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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.
| Autores principales: | , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Springer Vienna
2019
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7220887/ https://www.ncbi.nlm.nih.gov/pubmed/32421059 http://dx.doi.org/10.1007/s00605-019-01332-3 |