A continuously stratified nonlinear model for internal solitary waves in the northern South China Sea
Xie, JS ; Cai, SQ ; He, YH
刊名CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY
2010
卷号28期号:5页码:1040-1048
关键词internal solitary waves numerical modeling sill South China Sea
ISSN号0254-4059
通讯作者caisq@scsio.ac.cn
中文摘要A continuously stratified nonlinear model is set up to study the impact of topographical character on the generation of internal solitary waves over a sill by tidal flow. One of the reasons why almost all of the generated internal solitary waves propagate westward in the northern South China Sea is explained. The model simulations describe the generation and propagation of internal waves well. When the strength of imposed barotropic tides and the water stratification stay unchanged, the steepness of the sill slope can control both (a) whether or not the waves induced over a sill by tidal flow are linear internal waves or nonlinear internal solitary waves, and (b) the amplitude of the internal solitary waves generated. If the steepness of the sill is asymmetric, the nonlinear internal solitary waves may be induced on the steeper side of the sill. These conclusions are supported by a numerical experiment with a monthly-mean stratification and an actual seafloor topography from the Luzon Strait.
学科主题Limnology; Oceanography
收录类别SCI
原文出处SCIENCE PRESS
WOS记录号WOS:000281711600012
公开日期2011-07-03
内容类型期刊论文
源URL[http://ir.scsio.ac.cn/handle/344004/6241]  
专题南海海洋研究所_热带海洋环境国家重点实验室(LTO)
推荐引用方式
GB/T 7714
Xie, JS,Cai, SQ,He, YH. A continuously stratified nonlinear model for internal solitary waves in the northern South China Sea[J]. CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY,2010,28(5):1040-1048.
APA Xie, JS,Cai, SQ,&He, YH.(2010).A continuously stratified nonlinear model for internal solitary waves in the northern South China Sea.CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY,28(5),1040-1048.
MLA Xie, JS,et al."A continuously stratified nonlinear model for internal solitary waves in the northern South China Sea".CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY 28.5(2010):1040-1048.
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