A layered numerical model for simulating the generation and propagation of internal tides over continental slope III. Numerical experiments and simulation

Du Tao; Fang Xin-hua; Fang Guo-hong

doi:10.1007/BF02842537

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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

OriginalPaper | Updated：2023-05-16

- A layered numerical model for simulating the generation and propagation of internal tides over continental slope III. Numerical experiments and simulation
- A layered numerical model for simulating the generation and propagation of internal tides over continental slope III. Numerical experiments and simulation
- 海洋湖沼学报（英文） 2000年18卷第1期页码：18-24
- Affiliations：
  
  1. Institute of Oceanology Chinese Academy of Sciences
  2. Physical Oceanography Institute Ocean University of Qingdao
- Author bio：
- Funds：
  
  Contribution No. 3590 from the Institute of Oceanology, Chinese Academy of Sciences.;Project 49676275 supported by NSFC and also supported by National Special Research Program 97-926-05-02.
- DOI：10.1007/BF02842537
  中图分类号：
- 纸质出版：2000
- Accepted：
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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[J]. 海洋湖沼学报（英文）, 2000,18(1):18-24.

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
A layered numerical model for simulating the generation and propagation of internal tides over continental slope III. Numerical experiments and simulation[J]. 海洋湖沼学报（英文）, 2000,18(1):18-24. DOI： 10.1007/BF02842537.

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：

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.

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references

Fang Guohong, 1986. Tide and tidal current charts for the marginal seas adjacent to China.Chin. J. Oceanol. Limnol. 4(1): 1–16.

Holloway, P. E., 1996. A numerical model of internal tides with application to the Australian north west shelf.J. Phys. Oceanogr. 26: 21–37.

Martinsen, E. A., Engedahl, H., 1987. Implementation and testing of a lateral boundary scheme as an open boundary condition in a barotropic ocean model.Coastal Eng. 11: 603–627.

Rattary, M. Jr., 1960. On the coastal generation of internal tides.Tellus 12: 54–62.

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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