Tide response and tidal wave distortion in the Xianshan Bay Ⅲ. Numerical modelling study in a ideal rectangular bay

Dong Lixian; Su Jilanic; Wong Li Ah

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Dong Lixian, Su Jilanic, Wong Li Ah. Tide response and tidal wave distortion in the Xianshan Bay Ⅲ. Numerical modelling study in a ideal rectangular bay[J]. Haiyang Xuebao, 1999, 21(3): 1-6.

Citation:

Dong Lixian, Su Jilanic, Wong Li Ah. Tide response and tidal wave distortion in the Xianshan Bay Ⅲ. Numerical modelling study in a ideal rectangular bay[J]. Haiyang Xuebao, 1999, 21(3): 1-6.

Dong Lixian, Su Jilanic, Wong Li Ah. Tide response and tidal wave distortion in the Xianshan Bay Ⅲ. Numerical modelling study in a ideal rectangular bay[J]. Haiyang Xuebao, 1999, 21(3): 1-6.

Citation:

Dong Lixian, Su Jilanic, Wong Li Ah. Tide response and tidal wave distortion in the Xianshan Bay Ⅲ. Numerical modelling study in a ideal rectangular bay[J]. Haiyang Xuebao, 1999, 21(3): 1-6.

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Tide response and tidal wave distortion in the Xianshan Bay Ⅲ. Numerical modelling study in a ideal rectangular bay

1.
Second institute of Ocmnography, State Oceanic Administration, Hangzhou 310012
2.
Hong Kong Un University fo Science and Technology, Kowloon, Hong Kong

Received Date: 1997-11-08
Rev Recd Date: 1998-06-18

Abstract

Abstract

The contribution of the tidal flat and tidal currents advection to the generation and growth of M₄ tidal component is analyzed by using a numerical modelling in a ideal semi-enclosed rectanglular bay. The result shows that the contribution of tidal flat depends not only on the location and dimension of the tidal flat, but also on the non-linearity of the tide in the bay. The amplitude of the My tidal component is inhibited by the advection in the bay where there is the M₄ tide co-oscillation.
- M₄ tide,
- numerical modelling,
- co-oscillation,
- advection

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References(16)

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