Topographic Steering of the Upper Arctic Ocean Circulation by Deep Flows
Dynamically, the Arctic Ocean is characterised by the presence of closed f/H contours, where f is the Coriolis parameter and H the depth. On closed f/H contours, a net integrated surface wind stress can theoretically drive relatively strong near-bottom flows. Nevertheless, the Rossby number of the l...
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| Principais autores: | , , |
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| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
Stockholm University Press
2024-11-01
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| coleção: | Tellus: Series A, Dynamic Meteorology and Oceanography |
| Assuntos: | |
| Acesso em linha: | https://account.a.tellusjournals.se/index.php/su-j-tadmo/article/view/4072 |
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