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Fate of three major rivers in the bohai Sea: A model study

机译:渤海三大河流命运的模式研究

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Huanghe (Yellow River), Haihe and Liaohe are three major rivers flowing into the Bohai Sea and account for more than 80% of the freshwater and land-drained material inputs annually. The fate of three rivers in the seawaters correlates with the transport and distribution of the riverine sediments and nutrients, and further exerts a profound influence on the local marine ecosystem dynamics. Therefore, the evolution of the river plumes under the influence of the freshwater buoyancy, the tidal forcing and the wind stress are examined using a three-dimensional primitive equation ocean circulation model, independently and jointly. It is found that both tide and wind stirring can deteriorate the stabilization of the water column caused by the freshwater buoyancy; however, the processes are different. The tide stirring originates from the seafloor due to the bottom friction as the tidal wave propagates into the shallow waters, and then the turbulent kinetic energy dissipates upward. On the other hand, the wind stirring proceeds in the up-down direction. The influences of different winds on the evolution of the river plumes are also examined. Since the situation of each river mouth is different, the wind influence is also distinct. At last, the fate of three major rivers driven by the combined tidal forcing and climatology winds is reproduced, and the simulated salinity distribution shows a reasonable agreement with that observed, meaning that the river plume evolution plays a crucial role in shaping the salinity distribution in BS.
机译:黄河(黄河),海河和辽河是流入渤海的三大主要河流,每年占淡水和陆地排水物资投入的80%以上。海水中的三条河流的命运与河流沉积物和养分的运输和分布有关,并进一步影响了当地海洋生态系统的动态。因此,利用三维原始方程海洋环流模型,独立地和共同地研究了在淡水浮力,潮汐强迫和风应力的影响下河羽的演变。已经发现,潮汐和风的搅拌都会破坏由淡水浮力引起的水柱的稳定性。但是,过程不同。当潮汐传播到浅水区时,由于底部摩擦,潮汐搅动起源于海床,然后湍流动能向上消散。另一方面,风搅拌沿上下方向进行。还检查了不同风向对河羽演化的影响。由于每个河口的情况不同,因此风的影响也不同。最后,重现了潮汐强迫和气候风共同驱动的三大河流的命运,模拟的盐分分布与观测到的盐分具有合理的一致性,这意味着河流羽流的演变在塑造盐分中起着至关重要的作用。 BS。

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