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A parabolic model of drag coefficient for storm surge simulation in the South China Sea
Drag coefficient (C(d)) is an essential metric in the calculation of momentum exchange over the air-sea interface and thus has large impacts on the simulation or forecast of the upper ocean state associated with sea surface winds such as storm surges. Generally, C(d) is a function of wind speed. How...
| Autores principales: | , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
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Nature Publishing Group
2015
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| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4620453/ https://www.ncbi.nlm.nih.gov/pubmed/26499262 http://dx.doi.org/10.1038/srep15496 |