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Study on circulation and meso-scale eddies in the South China Sea in summer of 1998

机译:1998年夏季南海环流和中尺度涡的研究

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摘要

By using wide scope ADCP data which were got during SCSMEX (South China Sea Monsoon Experiment) period in the summer of 1998, and comparing these data with numerical modelling result, the distribution and variation characteristics of the circulation and meso-scale eddies in the South China Sea (SCS) were studied. The results show that: (1) in the SCS, 18 different scale eddies or motion systems with characteristics similar to meso-scale eddy were found during the investigation; (2) a strong westward current was found in the south of the Taiwan Shoal; (3) the energy of those eddies west of 114°E was much stronger than that of the east; and (4) there exist many powerful meso-scale eddies in the Nansha region south of 12°N. The distributions of numerous eddies reflect the complexity of the circulation in the SCS. It seems that the formation of those eddies should be caused by joint work of wind, coast feature, bottom topography, water density, inertial force and continental shelf waves.
机译:通过使用1998年夏季SCSMEX(南海季风实验)期间获得的广泛ADCP数据,并将这些数据与数值模拟结果,南部地区环流和中尺度涡旋的分布和变化特征进行比较。研究了中国海(SCS)。结果表明:(1)在南海调查中发现了18种不同尺度的涡旋或运动系统,其特征与中尺度涡旋相似。 (2)在台湾浅滩南部发现强烈的西风; (3)114°E以西的涡流的能量比东方的强得多; (4)在北纬12°以南的南沙地区存在许多强大的中尺度涡旋。涡流的分布反映了南海环流的复杂性。这些涡流的形成似乎应该是由风,海岸特征,底部地形,水密度,惯性力和大陆架波的共同作用引起的。

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