The Residual Current Derived from Ship-board ADCP Measurements of East China Sea in June 1999
碩士 === 國立臺灣大學 === 海洋研究所 === 93 === In most shallow seas, the major components of ocean current are tides. To derive the residual low frequency current velocity, one usually deploys current meter moorings over 25 hours or more to remove the diurnal and semi-diurnal tidal components. Using ship-board...
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| Format: | Others |
| Language: | zh-TW |
| Published: |
2005
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| Online Access: | http://ndltd.ncl.edu.tw/handle/24565836741299631346 |