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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...
Uloženo v:
| Vydáno v: | Sci Rep |
|---|---|
| Hlavní autoři: | , |
| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
Nature Publishing Group
2015
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| Témata: | |
| On-line přístup: | https://ncbi.nlm.nih.gov/pmc/articles/PMC4620453/ https://ncbi.nlm.nih.gov/pubmed/26499262 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/srep15496 |
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