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Schubert, René; Gula, Jonathan; Greatbatch, Richard J.; Baschek, Burkard; Biastoch, Arne. |
Mesoscale eddies can be strengthened by the absorption of submesoscale eddies resulting from mixed layer baroclinic instabilities. This is shown for mesoscale eddies in the Agulhas Current system by investigating the kinetic energy cascade with a spectral and a coarse-graining approach in two model simulations of the Agulhas region. One simulation resolves mixed layer baroclinic instabilities and one does not. When mixed layer baroclinic instabilities are included, the largest submesoscale near-surface fluxes occur in wintertime in regions of strong mesoscale activity for upscale as well as downscale directions. The forward cascade at the smallest resolved scales occurs mainly in frontogenetic regions in the upper 30 m of the water column. In the Agulhas... |
Tipo: Text |
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Ano: 2020 |
URL: https://archimer.ifremer.fr/doc/00644/75652/76523.pdf |
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