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Tidal Simulation in the East China Sea with Finite Element Method

机译:有限元法在东中国海的潮汐模拟

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摘要

A finite element model;;QUODDY model;;is used to study the tides inrnthe East China Sea;;the Yellow Sea and the Bohai Sea in this paper.rnThe simulation results fit well with the observation data. The cotidalrncharts of M2;;S2;;K1;;O1 and M4 are given out. The result of this paperrnsupports that the phase-lag of M2 varies little at Laizhou Bay. Thernamphidromic point of M2 disappears in the Liaodong Bay when thernbottom stress drag coefficient increases to 0.0028. There is a highrnamplitude (more than 0.06m) region of M4 around (32.8°N;;124.8°E).
机译:本文利用有限元模型QUODDY模型研究了东海,黄海和渤海的潮汐。模拟结果与观测数据吻合良好。给出了M2 ;; S2 ;; K1 ;; O1和M4的余弦图。本文的结果支持了莱州湾M2的相位滞后变化不大。当底应力阻力系数增加到0.0028时,辽东湾M2的高温点消失。在(32.8°N ;; 124.8°E)附近有一个M4的高振幅区域(大于0.06m)。

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