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廉州湾潮流和风海流的数值计算
引用本文:陈波,侍茂崇.廉州湾潮流和风海流的数值计算[J].广西科学,1996,3(3):32-35.
作者姓名:陈波  侍茂崇
作者单位:[1]广西海洋研究所 [2]青岛海洋大学
摘    要:对廉州湾潮流及风海流的数值计算结果显示,廉州湾落潮流大于涨潮流,最大落潮流速78cm/s,最大涨潮流速55cm/s,强流区位于北海市地角镇以外海域,风海流随风向不同改变,当海面盛行西南风时,海水流向湾内东北部,至湾顶沿岸后返向西南流动,当海面盛行东风及东南风时,海水又向西流动,以上结果与实资料基本吻合。

关 键 词:潮流  风海流  数值计算  廉州湾
收稿时间:1996/7/1 0:00:00

Numerical Calculation about the Tidal Current and Wind Current in the Lianzhou Bay
Chen Bo and Shi Maochong.Numerical Calculation about the Tidal Current and Wind Current in the Lianzhou Bay[J].Guangxi Sciences,1996,3(3):32-35.
Authors:Chen Bo and Shi Maochong
Institution:Guangxi Institute of Oceanography, East Nanzhu Road, Beihai, Guangxi, 536000 and Ocean University of QingDao, QingDao, Shandong, 266003
Abstract:According to the numerical calculation Of tidal current and wind current Of Lianzhou Bay, the ebb current velocity is greater than the find current velocity. And the maxima ebb is 78 cm/s, flood 55 cm/s. The strong current zone lies in the sea area out of the town of Dijiao.wind current changes with wind direction. As southwest wind blowig,sea water flows to the northeast of the Bay, and changes to flow to the southwest after it reaches the shoreline of the Bay head.While east wind and southeast wind blowing, it flows to west. The above results are almost in accordance with the survey data.
Keywords:tidal current  wind current  numerical calculation  Lianzhou bay
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