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- W2053148063 abstract "A two-layered finite difference model is developed for the Taiwan Strait, which in reality is exposed to a rectilinear monsoonal wind field in the presence of persistent stratification. In summer, upwelling is known to occur and this is concentrated on the Xiamen-Shantou coast, rather than along the length of the Strait. This feature is readily reproduced by the model and the concentration is shown to be dependent upon the bottom topography. The winter condition is more complex because the upwelling is observed to occur in mid-shelf. This feature is only reproduced when the Kuroshio Current is introduced into the model, travelling north-eastwards in opposition to the seasonal wind, and interacting with the bottom topography. Given a north-east monsoon wind averaging 7 m s−1, considered appropriate for the Strait, a Kuroshio Current of minimum strength of one knot is required to reproduce the mid-shelf upwelling. The strong influence of bottom topography is discussed together with the nonlinear features of wind stress and the occurrence of smaller scale topographically controlled features. The model resolves some local controversies concerning the basic marine dynamics of the area, and yet relies upon only sketchy meteorological and physical marine data. The provision of more experimental information holds much promise for a detailed understanding of the fundamental physics of the Taiwan Strait." @default.
- W2053148063 created "2016-06-24" @default.
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- W2053148063 date "1988-01-01" @default.
- W2053148063 modified "2023-10-18" @default.
- W2053148063 title "Upwelling in the Taiwan Strait in response to wind stress, ocean circulation and topography" @default.
- W2053148063 cites W2042101557 @default.
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- W2053148063 doi "https://doi.org/10.1016/0272-7714(88)90009-1" @default.
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