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引用本文:尹宝树,王涛,侯一筠,程明华,范顺庭,苏京志,M.I.ElSabh.渤海波浪和潮汐风暴潮相互作用对波浪影响的数值研究.海洋与湖沼,2001,32(1):109-116.
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渤海波浪和潮汐风暴潮相互作用对波浪影响的数值研究
尹宝树1, 王涛1, 侯一筠1, 程明华1, 范顺庭1, 苏京志1, M.I.ElSabh2
1.中国科学院海洋研究所 青岛266071;2.加拿大魁北克大学 里木斯基G5L,3A1
摘要:
基于依赖波浪成长状态波令的表面风应力,提出了一个波浪和风暴潮潮汐运动相互作用的联合数值模式,实现了第三代波浪模式和三维风暴潮潮汐模式联合作用的数值研究,并结合渤海典型天气个例的研究,给出了渤海波浪和风暴潮潮汐相互作用对波浪影响的机制和大小量级的定量估计。研究表明,对不同天气过程,波浪和风暴潮潮汐相互作用对波浪影响的性质和大小不同;对强寒潮过程,对波浪影响主要由风暴潮所支配,波高调制可达1m,在黄河口区一般达0.5m;对弱天气过程,对波浪影响主要由潮所控制,波高调制约在0.2m,联合作用模式给出的结果与实测更吻合。
关键词:  渤海  波潮风暴潮  联合数值模式  影响机制  定量估计
DOI:
分类号:
基金项目:国家“九五”攻关课题,D48970108号;中国科学院重点项目,A16970110号
附件
NUMERICAL STUDY OF THE INFLUENCE OF WAVES AND TIDE SURGE INT ERACTION ON WAVES IN BOHAI SEA
YIN Bao-Shu1, WANG Tao1, HOU Yi-Jun1, CHENG Ming-Hua1, FAN Shun-Ting1, SU Jing-Zhi1, M.I.ElSabh2
1.Institute of Oceanology,The Chinese Academy of Sciences,Qingdao,266071;2.University of Quebec at Rimouski,Rimouski,G5L,3A1,Canada
Abstract:
This paper developed a joint numerical model of wave and tide-surge motion. The model consists of an advanced third generation shallow water wave model and a three dimensional tide-surge model, taking into account all wave-current interactions and time varying depth. The joint interaction was carried out by running the two models interactively, exchanging calculated data of sea parameters at regular time intervals. The joint model was applied to the Bohai Sea. For the typical weather cases, influence mechanisms of wave and tide-surge interaction on waves and quantitative estimates of magnitude were obtained. The results demonstrate that the influence nature and magnitude vary with weather conditions; for the cases of moderate intensity, the effects of wave-tide-surge interaction on waves are mainly dominated by tides, but for strong cold waves, the effects of wave-tide-surge interaction on waves are mainly dominated by storm surges and in these cases both storm elevation and currents have some effects on waves, to a certain degree. At the Huanghe River mouth, the effects of storm set up and currents on waves are inverse and partially cancel out, weakening the interaction effects; in general, for strong cold wave cases, wave height maximum modulation can reach 1m, and at the Huanghe River estuary up to 0.5m; for weak weather cases, wave height maximum modulation is around 0.2m. The results computed by the joint model are in good agreement with measured data.
Key words:  Bohai sea, Wave-tide-surge, Combined numerical model, Influence mechanisms, Quantitative estimates
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