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A Mechanism of Seawater Exchange in Strait-Basin Systems in the Seto Inland Sea, Japan

机译:日本濑户内海海峡-盆地系统中的海水交换机制

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The seawater exchange is closely related to the spreading of pollutant and then water quality in coastal seas. The Seto Inland Sea is a semi-enclosed coastal sea which has a series of broad basins and narrow straits. There are several major driving forces of the seawater exchange between a strait and a basin; tide, wind and horizontal gradient of density. In this study, seawater exchange in a strait-basin system in the Seto Inland Sea was quantified by an observation using Acoustic Doppler Current Profiler (ADCP). A numerical model based on Princeton Ocean Model (POM) was also used in order to analyze the mechanisms of the seawater exchange. The observed residual current indicated the existence of the exchange flow across the boundary between the strait and basin; significant outflow from the strait to the surface layer of the basin. The exchange flow was well reproduced using the model which was driven by tide and horizontal density gradient between the strait and basin, suggesting that the seawater exchange was mainly induced by the interaction between tidal stirring and density current.
机译:海水交换与污染物的扩散以及沿海海域的水质密切相关。濑户内海是半封闭的沿海海域,拥有一系列宽阔的盆地和狭窄的海峡。海峡与流域之间的海水交换有几个主要的驱动力。潮,风和水平梯度的密度。在这项研究中,濑户内海海峡-海盆系统中的海水交换通过使用声学多普勒电流剖面仪(ADCP)的观测进行了定量。为了分析海水交换的机理,还使用了基于普林斯顿海洋模型(POM)的数值模型。观测到的剩余电流表明存在跨过海峡和盆地边界的交换流。从海峡到盆地表层的大量流出。利用海潮与海盆之间的潮汐和水平密度梯度驱动的模型很好地再现了交换流量,这表明海水交换主要是由潮汐搅动和密度流之间的相互作用引起的。

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