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Observed sub-inertial current variability and volume transport over the continental shelf in the northern South China Sea

机译:观测到南海北部大陆架上的亚惯性电流变化和体积输运

摘要

Sub-inertial currents (SICs) over the continental shelf of the northern South China Sea (NSCS) are investigated using the in-situ current observations of acoustic Doppler current profiler (ADCP) mooring arrays off the Pearl River Estuary in 2006 and 2007. The survey was carried out in four separate time periods: summer, winter, spring (before the onset of the southwesterly monsoon), and fall (after the establishment of the northeasterly monsoon). The observations showed that the current directions were generally along the shelf, consistent with the directions of monsoonal winds. The currents were also affected by a few of mesoscale eddy events. In summer 2006, the volume transport was northeastward with a mean magnitude of 1.4 Sv through a cross-shelf section from the site of the depth of 135 m to the coast; in winter 2006/2007, spring 2007 and fall 2007, the volume transports were all southwestward with magnitudes of 2.0, 2.1, and 0.9 Sv, respectively, through a cross-shelf section from the site of the depth of 290 m to the coast. The standard deviations of the SICs were generally smaller than the velocities of the mean currents, and the variability of SICs showed significant correlation with the local sea surface winds. No persistent counter-wind currents were observed in the study area during the fall and winter observational periods. (C) 2015 Elsevier Ltd. All rights reserved.
机译:利用2006年和2007年珠江口外的声多普勒电流剖面仪(ADCP)系泊阵列的原位电流观测,研究了南海北部大陆架(NSCS)上的亚惯性流(SIC)。调查在四个不同的时间段进行:夏季,冬季,春季(西南季风爆发之前)和秋季(东北季风建立之后)。观测结果表明,目前的风向大体上是沿着陆架,与季风风向一致。洋流还受到一些中尺度涡流事件的影响。在2006年夏季,从135 m深度站点到海岸的跨架断面向东北移动,平均幅度为1.4 Sv。在2006/2007年冬季,2007年春季和2007年秋季,从290 m深度站点到海岸的跨架剖面分别将体积运输量分别向西南移动,分别为2.0、2.1和0.9 Sv。 SIC的标准偏差通常小于平均海流的速度,并且SIC的变异性与当地海表风显着相关。在秋季和冬季的观测期内,研究区域未观察到持续的逆风流。 (C)2015 Elsevier Ltd.保留所有权利。

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