A layered numerical model for simulating the generation and propagation of internal tides over continental slope III. Numerical experiments and simulation
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A layered numerical model for simulating the generation and propagation of internal tides over continental slope III. Numerical experiments and simulation
Journal of Oceanology and LimnologyVol. 18, Issue 1, Pages: 18-24(2000)
Affiliations:
1. Institute of Oceanology Chinese Academy of Sciences
2. Physical Oceanography Institute Ocean University of Qingdao
Tao, D., Xin-hua, F. & Guo-hong, F. A layered numerical model for simulating the generation and propagation of internal tides over continental slope III. Numerical experiments and simulation., Chin. J. Ocean. Limnol. 18, 18–24 (2000). https://doi.org/10.1007/BF02842537
DOI:
Tao, D., Xin-hua, F. & Guo-hong, F. A layered numerical model for simulating the generation and propagation of internal tides over continental slope III. Numerical experiments and simulation., Chin. J. Ocean. Limnol. 18, 18–24 (2000). https://doi.org/10.1007/BF02842537DOI:
A layered numerical model for simulating the generation and propagation of internal tides over continental slope III. Numerical experiments and simulation
摘要
Abstract
The layered model in Part I was used to simulate the internal tide in a stratified
two layer
and rectangular sea area with step-like topography. The internal tide current velocities of the upper and lower layers and the interfacial elevations were computed and the effect of the upper layer water depth and density difference were studied. Numerical experiments verified that the model can correctly simulate internal tides. The model was also applied to the northwestern part of the South China Sea to simulate the internal tides there with real topography. The distributions of internal tide amplitude in interfaces were delineated.
关键词
Keywords
references
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Wilmott, A. J., Edwards, P. D., 1987. A numerical model for the generation of tidally forced nonlinear internal waves over topography.Contin. Shelf Res. 7: 457–484.
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