Tide response and tide wave distortion study in the Xiangshan Bay Ⅱ. Numerical modelling study in the Xiangshan Bay

Dong Lixian; Su Jilan

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Dong Lixian, Su Jilan. Tide response and tide wave distortion study in the Xiangshan Bay Ⅱ. Numerical modelling study in the Xiangshan Bay[J]. Haiyang Xuebao, 1999, 21(2): 1-8.

Citation:

Dong Lixian, Su Jilan. Tide response and tide wave distortion study in the Xiangshan Bay Ⅱ. Numerical modelling study in the Xiangshan Bay[J]. Haiyang Xuebao, 1999, 21(2): 1-8.

Dong Lixian, Su Jilan. Tide response and tide wave distortion study in the Xiangshan Bay Ⅱ. Numerical modelling study in the Xiangshan Bay[J]. Haiyang Xuebao, 1999, 21(2): 1-8.

Citation:

Dong Lixian, Su Jilan. Tide response and tide wave distortion study in the Xiangshan Bay Ⅱ. Numerical modelling study in the Xiangshan Bay[J]. Haiyang Xuebao, 1999, 21(2): 1-8.

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Tide response and tide wave distortion study in the Xiangshan Bay Ⅱ. Numerical modelling study in the Xiangshan Bay

Second Institute of Oceanography, State Ocean Administration, Hangzhou 310012

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

Abstract

Abstract

The mechanisms of M₄ tide component are analyzed by means of a tide modelling in the Xiangshan Bay.The result shows that the generating and developing processes of M₄ tide component are controlled mainly by the effects of the nonlinear bottom friction during the tide wave propagation.The M₄ tide co-oscillation is important to amplify the M₄ tide in the Xiangshan Bay.The effect of advection amplifies the M₄ tide only in the small individual area near some islands located in the Fudu Channel.The tidal flat has a little effect on the M₄ tide.
- Distortion,
- M₄ tide,
- numerical modellinx,
- Xiangshan Bay

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References(16)

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