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Chezy型和广义Manning型摩擦关系在渤、黄、东海陆架潮汐模拟中的应用
引用本文:滕飞,方国洪,魏泽勋,徐晓庆,崔欣梅,吴頔.Chezy型和广义Manning型摩擦关系在渤、黄、东海陆架潮汐模拟中的应用[J].海洋与湖沼,2016,47(4):696-705.
作者姓名:滕飞  方国洪  魏泽勋  徐晓庆  崔欣梅  吴頔
作者单位:中国海洋大学 青岛 266100,中国海洋大学 青岛 266100;国家海洋局第一海洋研究所 青岛 266061,国家海洋局第一海洋研究所 青岛 266061,国家海洋局第一海洋研究所 青岛 266061,国家海洋局第一海洋研究所 青岛 266061,国家海洋局第一海洋研究所 青岛 266061
基金项目:国家自然科学基金项目,40676009号,40606006号;中央级公益性科研院所基本科研业务费专项资金资助项目,2013G01号;青岛市科技计划基础研究项目,11-1-4-98-jch号。
摘    要:以往对渤、黄、东海潮汐数值模拟中使用的摩擦系数大都采用不随地点变化的常数,即采用Chezy型摩擦。为了改善模拟效果,本文比较了Chezy型和广义Manning型摩擦关系,并选择与实测数据符合最好的参数,即最优参数。结果表明,采用广义Manning型摩擦系数所得结果更好。底摩擦系数在0.0009至0.0014之间,显著低于Proudman(1953)给出的0.0026,也比以往大多数已发表的值小。与原始的Manning公式不同(该公式的幂值为负数),本研究得到的幂值为正,表明在渤、黄、东海陆架区。总体上,水体越浅摩擦系数越小。本文给出了根据最优Manning型摩擦参数模拟得出的同潮图和能通量分布图,并描述了它们的特征。

关 键 词:渤海  黄海  东海  数值模拟  海底摩擦
收稿时间:2015/12/28 0:00:00
修稿时间:3/7/2016 12:00:00 AM

TIDAL SIMULATION IN CHEZY-TYPE AND GENERALIZED MANNING-TYPE FRICTION FOR CHINESE EASTERN SHELF SEAS
TENG Fei,FANG Guo-Hong,WEI Ze-Xun,XU Xiao-Qing,CUI Xin-Mei and WU Di.TIDAL SIMULATION IN CHEZY-TYPE AND GENERALIZED MANNING-TYPE FRICTION FOR CHINESE EASTERN SHELF SEAS[J].Oceanologia Et Limnologia Sinica,2016,47(4):696-705.
Authors:TENG Fei  FANG Guo-Hong  WEI Ze-Xun  XU Xiao-Qing  CUI Xin-Mei and WU Di
Institution:Ocean University of China, Qingdao 266100, China,Ocean University of China, Qingdao 266100, China;The first Institute of Oceanography, SOA, Qingdao 266061, China,The first Institute of Oceanography, SOA, Qingdao 266061, China,The first Institute of Oceanography, SOA, Qingdao 266061, China,The first Institute of Oceanography, SOA, Qingdao 266061, China and The first Institute of Oceanography, SOA, Qingdao 266061, China
Abstract:Earlier numerical tidal simulations for Chinese eastern shelf seas (Bohai Sea, Yellow Sea, and East China Sea) often use a constant friction coefficient for all areas (the Chezy-type friction). We compared the Chezy-type with the generalized Manning-type friction, and chose the optimal parameters to fit best the observation. The results show that the modeling in the generalized Manning-type friction was more accurate than in the Chezy-type. In addition, the friction coefficients we recalculated for the study area range from 0.0009 to 0.0014, much smaller than 0.0026 given by Proudman in 1953 that often adopted previously. Different from the negative exponent in the original Manning formula, the exponent we obtained is positive, indicating that the shallower the water mass, the smaller the coefficient. In the generalized Manning-type, we reproduced cotidal charts and energy flux maps with new optimal parameters for the study area.
Keywords:Bohai Sea  Yellow Sea  East China Sea  numerical simulation  bottom friction
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