%0 Journal Article %T NUMERICAL STUDY ON THE TIDES AND TIDAL CURRENTS IN BOHAI SEA, YELLOW SEA AND EAST CHINA SEA
渤、黄、东海潮汐、潮流的数值模拟与研究 %A ZHU Xue-Ming %A BAO Xian-Wen %A SONG De-Hai %A QIAO Lu-Lu %A HUANG Bi-Gui %A SHI Xin-Gang %A
朱学明 %A 鲍献文 %A 宋德海 %A 乔璐璐 %A 黄必桂 %A 石新刚 %J 海洋与湖沼 %D 2012 %I %X A successful simulation for the tides and tidal currents has been done based on the Finite Volume Coastal Ocean Model (FVCOM) with unstructured triangle grids in high resolutions in Bohai Sea, Yellow Sea, and East China Sea. The numerical model agreed with the observation well by comparing the observed data with the simulation results from 120 gauge stations and 14 tidal currents stations. The distributions of the co-tidal charts, maximum velocity and co-range charts when maximum velocity occurs of the tidal currents in 5 meter layer are shown in this paper according to the model results, respectively. Model results indicatethat five semidiurnal and three diurnal constituents independent rotary tidal systems appear in Bohai Sea, Yellow Sea, and East China Sea, and they are all anti-clockwise; twelve tidal cur-rent-amphidromic points forsemidiurnal and diurnal constituents can be found, respectively; the four semidiurnal tidal current-amphidromic points located at the two sides of the Okinawa Island and Amami Island are symmetry, three of them are reported at first time; two diurnal tidal current-amphidromic points located in the west of Kyushu Island of Japan are reported at first time, too. But the existence of them should be validated by observation. %K Bohai Sea %K Yellow Sea %K East China Sea %K Tide %K Tidal current %K Numerical simulation %K FVCOM
渤海 %K 黄海 %K 东海 %K 潮汐 %K 潮流 %K 数值模拟 %K FVCOM %U http://www.alljournals.cn/get_abstract_url.aspx?pcid=E62459D214FD64A3C8082E4ED1ABABED5711027BBBDDD35B&cid=2D9C75573FA3E416&jid=10F18692CD69EACA2DF7FC109993D35C&aid=74204B17C4981C5A02F55CC9A90CCE68&yid=99E9153A83D4CB11&iid=B31275AF3241DB2D&sid=17FE7A1C78626A81&eid=0EFDF9DD0F63E842&journal_id=0029-814X&journal_name=海洋与湖沼&referenced_num=0&reference_num=0