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• W2375827061 abstract "Upwelling in coastal area of the East China Sea is an important phenomenon and raised extensive interests in this field. In order to understand the dynamic process and cause of vertical circulation in the area,based on real topography, surface wind stress, temperature and salinity distribution in this area, using 3D baroclinic ocean model, numerical simulations were performed for picturing vertical circulation and temperature/salinity patterns of wintertime and summertime. Results of the vertical circulation simulated are discussed in this paper. The numerical results of the vertical circulation demonstrated different patterns in wintertime and summertime. In wintertime, the vertical circulation in this area is counterclockwise, flowing shoreward in near-surface layer, downwelling in the coastal zones, and moving seaward below the surface layer with a rising tendency in outer sea. The current width of the shoreward current is narrow and its speed is strong. The current width of the seaward current is broad, and its speed is weak. The current width of the coastal downwelling is broader than that of the shoreward current and narrower than that of the seaward current. Its speed is weaker than that of the shoreward current, and is stronger than that of the seaward currents whose intensity gradually weakens with depth. In summertime, the vertical circulation there is clockwise being shoreward flow below the near-surface layer, upwelling in the coastal area, and seaward in the near-surface layer with a falling tendency in the outer sea. The current width of the shoreward current is broad, and its speed is weak. The current width of the seaward current is narrow, and its speed is strong. The current width of the coastal upwelling is narrower than that of the shoreward current and broader than that of the seaward currents. Its speed is stronger than that of the shoreward current, and is weaker than that of the seaward currents and gradually enhances from the bottom layer to the surface layer. As for whole coastal sea area, the intensity of the coastal downwelling increases gradually with increasing of continental slope, heightening of wind velocity, and decreasing of the angle between wind direction and coastline from the north to the south during the wintertime. The intensity of the coastal upwelling increases and then decreases gradually with decreasing of continental slope, increasing of wind velocity, and decreasing and then increasing of the angle between wind direction and coastline from the south to the north during the summertime. The continental slope, wind speed and the angle between wind direction and coastline influence the intensity of the coastal downwelling or upwelling, in which the angle between wind direction and coastline is a key factor for forming coastal downwelling or upwelling. The mechanism of the coastal downwelling is attributed mainly to coupling effects between the northeast wind and the coastline during the wintertime. However, the mechanism of the coastal upwelling is attributed mainly to coupling effects between the southwest wind and the coastline during the summertime." @default.
• W2375827061 created "2016-06-24" @default.
• W2375827061 creator A5030970629 @default.
• W2375827061 date "2004-01-01" @default.
• W2375827061 modified "2023-09-25" @default.
• W2375827061 title "DYNAMIC PROCESS OF VERTICAL CIRCULATION AND TEMPERATURE──SALINITY STRUCTURE IN COASTAL AREA OF EAST CHIAN SEA I. BASIC CHARACTERISTICS OF THE CIRCULATION" @default.
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