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Dampening of Submesoscale Currents by Air-Sea Stress Coupling in the Californian Upwelling System
Oceanic submesoscale currents (SMCs) occur on an scale of 0.1–10 km horizontally and have a large influence on the oceanic variability and on ecosystems. At the mesoscale (10–250 km), oceanic thermal and current feedbacks are known to have a significant influence on the atmosphere and on oceanic dyn...
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| Publicado no: | Sci Rep |
|---|---|
| Main Authors: | , , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
Nature Publishing Group UK
2018
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| Assuntos: | |
| Acesso em linha: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6127151/ https://ncbi.nlm.nih.gov/pubmed/30190530 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41598-018-31602-3 |
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