A steady stratified purely azimuthal flow representing the Antarctic Circumpolar Current
arXiv:2010.09389 · doi:10.1007/s00605-019-01332
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.