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Numerical study of seasonal circulation and variability over the inner shelf of the northern South China Sea

机译:南海北部内陆陆架季节性环流和变化的数值研究

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摘要

This study examines seasonal circulation, hydrography, and associated spatial variability over the inner shelf of the northern South China Sea (NSCS) using a nested-grid coastal ocean circulation model. The model external forcing consists of tides, atmospheric forcing, and open boundary conditions based on the global ocean circulation and hydrography reanalysis produced by the Hybrid Coordinate Ocean model. Five numerical experiments are conducted with different combinations of external forcing functions to examine main physical processes affecting the seasonal circulation in the study region. Model results demonstrate that the monthly mean circulation in the study region features the Guangdong Coastal Current (GCC) over coastal waters and the South China Sea Warm Current (SCSWC) in the offshore deep waters. The GCC produced by the model flows nearly southwestward in winter months and northwestward in summer months, which agrees with previous studies. The SCSWC flows roughly northeastward and is well defined in summer months. In winter months, by comparison, the SCSWC is superseded by the southwestward strong wind-driven currents. Analysis of model results in five different experiments demonstrates that the monthly mean circulation over coastal and inner shelf waters of the NSCS can be approximated by barotropic currents forced by the southwestward monsoon winds in winter months. In summer months, by comparison, the monthly mean circulation in the study region is affected significantly by baroclinic dynamics associated with freshwater runoff from the Pearl River and advection of warm and saline waters carried by the SCSWC over the NSCS.
机译:这项研究使用嵌套网格沿海海洋环流模型研究了南海北部内陆架(NSCS)的季节性环流,水文学以及相关的空间变化。基于混合坐标海洋模型产生的全球海洋环流和水文学重新分析,外部强迫模型由潮汐,大气强迫和开放边界条件组成。使用外部强迫函数的不同组合进行了五个数值实验,以检查影响研究区域季节性循环的主要物理过程。模型结果表明,研究区域的月平均环流具有沿海水域的广东沿海海流(GCC)和近海深水区域的南海暖流(SCSWC)。该模型产生的GCC在冬季月份几乎向西南流动,而在夏季月份则向西北流动,这与以前的研究一致。 SCSWC大致向东北流动,并在夏季得到明确定义。相比之下,在冬季,西南偏南SWSC被西南强风驱动的潮流所取代。在五个不同实验中对模型结果的分析表明,NSCS沿海和内陆水域的月平均环流可通过冬季冬季西南季风风强迫产生的正压流来近似。相比之下,在夏季,研究区域的月平均环流受斜压动力学的影响很大,这些动力学与珠江河淡水径流以及SCSWC在NSCS上携带的温水和盐水的平流有关。

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