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Bottom cold water (BCW) is widely reported to occur in many coastal areas in summer. Some BCW masses have an increase in temperature of only 1 °C from early spring to summer (e.g., North Sea, Yellow Sea), while the others have a 4–10 °C increase (e.g., Irish Sea, Seto Inland Sea). A model of heat transport with vertical diffusion alone gave good approximation of the temperature increase in the North...
A three-dimensional tidal current model is developed and applied to the East China Sea (ECS), the Yellow Sea and the Bohai Sea. The model well reproduces the major four tides, namely M2, S2, K1 and O1 tides, and their currents. The horizontal distributions of the major four tidal currents are the same as those calculated by the horizontal two-dimensional models. With its high resolutions in the horizontal...
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