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Water Masses in the South China Sea and Water Exchange between the Pacific and the South China Sea

机译:南中国海的水团和太平洋与南中国海之间的水交换

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摘要

Water masses in the South China Sea (SCS) were identified and analyzed with the data collected in the summer and winter of 1998. The distributions of temperature and salinity near the Bashi Channel (the Luzon Strait) were analyzed by using the data obtained in July and December of 1997. Based on the results from the data collected in the winter of 1998, waters in the open sea areas of the SCS were divided into six water masses: the Surface Water Mass of the SCS (S), the Subsurface Water Mass of the SCS (U), the Subsurface-Intermediate Water Mass of the SCS (UI), the Intermediate Water Mass of the SCS (I), the Deep Water Mass of the SCS (D) and the Bottom Water Mass of the SCS(B). For the summer of 1998, the Kuroshio Surface Water Mass (KS) and the Kuroshio Subsurface Water Mass (KU) were also identified in the SCS. But no Kuroshio water was found to pass the 119.5°E meridian and enter the SCS in the time of winter observations. The Sulu Sea Water (SSW) intruded into the SCS through the Mindoro Channel between 50-75 m in the summer of 1998. However, the data obtained in the summer and winter of 1997 indicated that water from the Pacific had entered the SCS through the northern part of the Luzon Strait in these seasons, but water from the SCS had entered the Pacific through the southern part of the Strait. These phenomena might correlate with the 1998 El-Nino event.
机译:利用1998年夏季和冬季收集的数据,对南海(SCS)的水体进行了识别和分析。利用7月份获得的数据分析了巴什海峡(吕宋海峡)附近的温度和盐度分布。和1998年12月。根据1998年冬季收集的数据结果,南海的公海区域的水被分为6个水体:南海的地表水体(S),地下水体SCS(U),SCS的地下中间水量(UI),SCS的中间水量(I),SCS的深水量(D)和SCS的底水量( B)。在1998年夏季,南海地区还发现了黑潮地表水团(KS)和黑潮地表水团(KU)。但是,在冬季观测时,没有发现黑潮水通过119.5°E子午线并进入南海。苏鲁海水(SSW)于1998年夏季在50-75 m之间通过Mindoro通道侵入南海。但是,1997年夏季和冬季获得的数据表明,来自太平洋的水已通过南太平洋进入南海。在这些季节中,吕宋海峡的北部,但是来自南海的水已经通过海峡的南部进入太平洋。这些现象可能与1998年的El-Nino事件有关。

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