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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...
| Autores principales: | , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
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Nature Publishing Group UK
2018
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| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6127151/ https://www.ncbi.nlm.nih.gov/pubmed/30190530 http://dx.doi.org/10.1038/s41598-018-31602-3 |