Enhanced Vertical Mixing in Coastal Upwelling Systems Driven by Diurnal‐Inertial Resonance: Numerical Experiments
Résumé
The land-sea breeze is resonant with the inertial response of the ocean at the critical latitude of 30 degrees N/S. 1-D vertical numerical experiments were undertaken to study the key drivers of enhanced diapycnal mixing in coastal upwelling systems driven by diurnal-inertial resonance near the critical latitude. The effect of the land boundary was implicitly included in the model through the "Craig approximation" for first-order cross-shore surface elevation gradient response. The model indicates that for shallow water depths (
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https://hal.univ-brest.fr/hal-02544118
Soumis le : vendredi 8 octobre 2021-08:40:53
Dernière modification le : dimanche 17 mars 2024-17:28:03
Archivage à long terme le : dimanche 9 janvier 2022-18:15:57
Citer
Giles Fearon, Steven Herbette, Jennifer Veitch, Gildas Cambon, Andrew Lucas, et al.. Enhanced Vertical Mixing in Coastal Upwelling Systems Driven by Diurnal‐Inertial Resonance: Numerical Experiments. Journal of Geophysical Research. Oceans, 2020, 125 (9), ⟨10.1029/2020JC016208⟩. ⟨hal-02544118v1⟩
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