首页 | 本学科首页   官方微博 | 高级检索  
     检索      

东中国海潮余流自适应数值模拟
引用本文:周旭波,孙文心,苏健.东中国海潮余流自适应数值模拟[J].中国海洋大学学报(自然科学版),2002,32(2):173-178.
作者姓名:周旭波  孙文心  苏健
作者单位:青岛海洋大学物理海洋研究所,青岛,266003
基金项目:国家自然科学基金重点项目 ( 4 9736 1 90 ),国家自然科学基金 ( 4 0 0 76 0 0 2 ),国家 973项目 ( G1 9990 4 370 3)
摘    要:以自适应数值模型首次计算整个东中国海三维 M2 分潮潮致 Euler余流、Stokes漂流和L agrange余流 ,并分析各海区 L agrange余流的特征。渤海 M2 分潮致 L agrange余流在整个海域基本形成一个大的逆时针环流系统 ;辽东湾有一个逆时针流环。在黄海 ,潮致余流也是黄海环流的重要组成部分。在东海的东北部 ,潮致余流有强化对马暖流的作用 ;在台湾北部海域 ,潮余流对台湾暖流有强化作用。在近海海域 ,由于复杂地形的作用 ,潮流非线性作用加强 ,潮余流的量值有较明显的增加。计算结果表明 :在浅水区域 ,Stokes漂流较大 ,Euler余流与 Lagrange余流差别显著

关 键 词:东中国海  潮余流  Lagrange余流  自适应  数值模拟
文章编号:1001-1862(2002)02-173-06
修稿时间:2001年5月29日

Self-Adaptive Numerical Simulation of Tide-Induced Residual Current in the East China Sea
Zhou Xubo\ Sun Wenxin\ Su Jian.Self-Adaptive Numerical Simulation of Tide-Induced Residual Current in the East China Sea[J].Periodical of Ocean University of China,2002,32(2):173-178.
Authors:Zhou Xubo\ Sun Wenxin\ Su Jian
Abstract:Self adaptive numerical model is used to simulate the 3 D tide induced Euler, Stokes and Lagrangian residual currents in the East China Sea for the first time.The character of Lagrangian residual current in each area is analysed. In the Bohai Sea, Lagrangian residual current of the M 2 tide basically forms a large anticlockwise circulation; there is an anticlockwise circulation in the Liaodong Bay. In the Huanghai Sea, tide induced residual current is also an important part of its circulation. In the northeast part of the East Sea, tide reduced current makes Tsushima Warm Current stronger. In the area northern of Taiwan, tide reduced current makes Taiwan Warm Current stronger. In the coastal seas, the nonlinear interaction of tide and tide reduced current are stronger due to the comflex topography. The results show that stokes residual current is stronger in shallow seas, and Euler residual current is very different from Lagrangian residual current.
Keywords:the East China Sea  tide  induced residual current  Lagrangian residual current  self  adaptive  numerical simulation
本文献已被 CNKI 万方数据 等数据库收录!
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号