How high frequency atmospheric forcing impacts mesoscale eddy surface signature and vertical structure
Résumé
• Seasonal variations in SST and mixed layer anomalies of a Mediterranean anticyclone are retrieved in high resolution simulation • The summer surface cold-core signatures are driven by differential vertical mixing due to near-inertial waves • SST retroaction on air-sea fluxes is necessary to retrieve eddy-induced mixed layer anomalies
Domaines
OcéanographieOrigine | Fichiers produits par l'(les) auteur(s) |
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