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Interannual Variation of Freshwater in the Yellow and East China Seas: Roles of the Changjiang Discharge and Wind Forcing

机译:黄海和东海淡水的年际变化:长江流量和强迫风的作用

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The interannual variation of the behavior of Changjiang freshwater has been investigated using the Princeton Ocean Model (POM). Five experiments are described in this study. Three basic experiments (Exps. B1, B2 and B3) were performed to examine the freshwater behavior in response to annual variations of the Changjiang discharge in normal, wet and dry years, respectively. Thereafter, the freshwater variation was investigated with the model forced by primary-interannual variations of river discharge with an 8-year period (Exp. I1) and a wind field with a 3.6-year period (Exp. I2). In Exp. B1, the average residence time of freshwater is roughly estimated to be 681.4 days in the Yellow Sea (YS) and 353.4 days in the combined area of the East China Sea (ECS) and the Chinese Coast (CC). This difference is attributed to the current pattern in each region and freshwater exchange among the regions. The interannual variation of freshwater volume in Exp. I1 has a large amplitude and long phase lag in the YS (38 km~3 and 1.6-year against primary-interannual discharge variation), while there are relatively small amplitudes and short phase lags in the ECS (18 km~3 and 0.7-year) and the CC (14 km~3 and 0.5-year). It is concluded that the difference in the freshwater behavior results from the difference in the average residence time in each region.
机译:使用普林斯顿海洋模型(POM)研究了长江淡水行为的年际变化。这项研究描述了五个实验。进行了三个基本实验(实验B1,B2和B3),分别检查正常,湿润和干旱年份长江水排放量年变化的淡水行为。此后,通过模型研究了淡水的变化,该模型是由河流排放量为8年(实验I1)和风场为3.6年周期(实验I2)的初次-年际变化所引起的。在实验中在B1中,黄海(YS)的淡水平均停留时间粗略估计为681.4天,东海(ECS)和中国海岸(CC)的合并区域淡水的平均停留时间约为353.4天。这种差异归因于每个区域的当前模式以及区域之间的淡水交换。 Exp中淡水量的年际变化。 I1在YS处具有较大的振幅和较长的相位滞后(38 km〜3和1.6年相对于一次年际流量变化),而在ECS中具有相对较小的振幅和较短的相位滞后(18 km〜3和0.7-年)和CC(14 km〜3和0.5年)。结论是,淡水行为的差异是由每个区域的平均停留时间的差异引起的。

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