Modeled wind-driven flow over the California continental shelf in terms of a local and a remote response
Previous results suggest that many higher order coastally trapped wave (CTW) modes are needed to calculate the low-frequency wind-driven alongshore flow over the continental shelf. Large mode number CTW asymptotics suggest that the higher order modes are generated by just the local wind. It is there...
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| Format: | Others |
| Language: | English |
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| Online Access: |
http://purl.flvc.org/fsu/lib/digcoll/etd/3161934 |