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Hydrological analysis of Kuroshio water intrusion into the South China Sea

机译:黑潮水浸入南海的水文分析

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摘要

Using CTD and ADCP data collected by four research vessels from both sides of the Taiwan Strait in the northeastern area of the South China Sea in August-September 1994 and incorporating With CTD data collected in the same area in March 1992 and some historical hydrologic data, the water Features and the intrusion of Kuroshio water into the South China Sea are discussed, which shows that The water mass distribution in the survey period was similar to that in the cruise of late winter and early Spring (March 1992), that is, the water structure in the northeast of the sea and in the Northwest Pa- Cific had their own independent features of temperature and salinity. Though the intrusion of Kuroshio Water into the sea was found, it was very weak. Therefore there would beno direct Kuroshio branch in- To the sea in the late summer and early autumn. Even the Kuroshio water intrusion from the Bashi Chan- Nel into the Taiwan Strait,its influence was also very weak.
机译:利用1994年8月至9月在南海东北部台湾海峡两岸四艘研究船收集的CTD和ADCP数据,并结合1992年3月在同一地区收集的CTD数据和一些历史水文数据,讨论了水的特征和黑潮对南中国海的入侵,表明调查期的水量分布与冬末和春初(1992年3月)的航行相似,即海洋东北部和西北太平洋的水结构具有各自独立的温度和盐度特征。尽管发现了黑潮水侵入海中,但非常微弱。因此,夏末和初秋将没有直接的黑潮分支入海。即使是黑潮从八十昌内尔侵入台湾海峡,其影响力也很弱。

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