On the Simulation of Shallow Water Tides in the Vicinity of the Taiwan Banks

The Taiwan Banks (Formosa Shoals), a large NE-SW oriented bathymetric feature near the southern end (23°N, 118 - 119°E) of the Taiwan Strait, is a region of extremely shallow water that exerts a profound effect on the propagation of tidal waves. As such waves propagate over the Taiwan Banks, they be...

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Bibliographic Details
Main Authors: Ming-Da Chiou, Hwa Chien, Luca R. Centurioni, Chia-Chuen Kao
Format: Article
Language:English
Published: Chinese Geoscience Union 2010-01-01
Series:Terrestrial, Atmospheric and Oceanic Sciences
Subjects:
Online Access: http://tao.cgu.org.tw/images/attachments/v211p027.pdf
Description
Summary:The Taiwan Banks (Formosa Shoals), a large NE-SW oriented bathymetric feature near the southern end (23°N, 118 - 119°E) of the Taiwan Strait, is a region of extremely shallow water that exerts a profound effect on the propagation of tidal waves. As such waves propagate over the Taiwan Banks, they become distorted and asymmetric due to bottom friction and contribute to the generation of shallow water tides. The POM model was used in present study to simulate the tides in the Taiwan Strait region. Shallow water tidal dynamics in the area of Taiwan Banks are focused. The numerical model was validated against sea level observations from 34 tidal stations located on the coast of Mainland China and Taiwan. Trajectory records from two SVP drifters are used to be compared with the simulations using wavelet-based rotary spectral analysis.
ISSN:1017-0839
2311-7680