摘要
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.
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.
基金
Project 4 96762 75supportedbyNSFCandalsosupportedbyNationalSpecialResearchProgram 97 92 6 0 5 0 2
