Using P0M97. an oceanic model, we separately do numerical tests to simulate the 3-D struc ture of temperature in the sea area around Taiwan Island with or without effect of Kuroshio (Current). Through contrast analysi...Using P0M97. an oceanic model, we separately do numerical tests to simulate the 3-D struc ture of temperature in the sea area around Taiwan Island with or without effect of Kuroshio (Current). Through contrast analysis. we find that inflow of Kuroshio results in winter mean water temperature of sub-surface layer in the whole sea regions raising 5 - 6℃ more than that without effect of Kuroshio. The existence of Kuroshio does important role on oceanic thermocline of deep water area in the east of Taiwan Island, and has some effect on intensity of seasonal thermocline of Taiwan Strait and its southern shallow water area.展开更多
文摘Using P0M97. an oceanic model, we separately do numerical tests to simulate the 3-D struc ture of temperature in the sea area around Taiwan Island with or without effect of Kuroshio (Current). Through contrast analysis. we find that inflow of Kuroshio results in winter mean water temperature of sub-surface layer in the whole sea regions raising 5 - 6℃ more than that without effect of Kuroshio. The existence of Kuroshio does important role on oceanic thermocline of deep water area in the east of Taiwan Island, and has some effect on intensity of seasonal thermocline of Taiwan Strait and its southern shallow water area.
