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盛夏南海的水文与环流特征:2000年8月航次再探
引用本文:李立,许金电. 盛夏南海的水文与环流特征:2000年8月航次再探[J]. 海洋学报, 2021, 0(6): 1-12. DOI: 10.12284/hyxb2021088
作者姓名:李立  许金电
作者单位:自然资源部第三海洋研究所 海洋动力学实验室,福建 厦门 361005
基金项目:国家重点研发计划(2016YFC1402607);科技基础资源调查专项(2017FY201402);国家重点基础研究发展规划项目(G1999043807)
摘    要:在国家重点基础研究发展规划的支持下,2000年8月在南海组织了1次多船同步海洋学调查,是迄今为止盛夏期间唯一一次全海盆准同步水文观测.航次间遭遇的多种困难虽被及时化解,然而观测数据的质量已受影响.此前虽已有若干相关研究发表,但未见对观测数据进行质量控制和全面的分析.本文在对CTD和ADCP原始数据仔细校正的基础上,分析...

关 键 词:南海  夏季环流  南沙反气旋环流  民都洛海峡
收稿时间:2020-09-14

Hydrography and circulation of the South China Sea in deep summer: The August 2000 cruises revisited
Affiliation:Laboratory of Marine Dynamics, Third Institute of Oceanography, Ministry of Natural Resources, Xiamen 361005, China
Abstract:Funded by the National Key Basic Research Development Program, a multi-vessel oceanography survey was conducted synoptically in the South China Sea (SCS) in August 2000, which appeared to be the unique, available synoptic survey that covered the entire SCS basin in deep summer. A number of difficulties were encountered during the survey that affected the quality of observation, even though they were resolved underway. Although some related research works were previously published, no carefully quality control of the data and a comprehensive analyses had ever appeared before. In this work, the original CTD and shipboard ADCP data were carefully calibrated in the first place, and the hydrography and circulation features were then analyzed and discussed to leave a record of the cruises as complete as possible. The results indicate that, in deep summer, the basin shows different physical characteristics on both sides of its SW–NE oriented axis of the basin. The circulation is generally anticyclonic southeast of the axis, in which the Nansha anticyclonic gyre (NSAG) is especially powerful; the area northwest of the axis, in contrast, appears to be dominated by mesoscale features of different categories, where no obvious structure of large scale circulation is found. The analyses confirm that the scales of the NSAG are over 400 km horizontally and nearly 1000 m vertically, with a maximal swirling speed close to 1 m/s, which appears to be the most remarkable circulation feature of the SCS. Moreover, its position and strength are subject to significant interannual variation. In the Mindoro Strait, the exchange flow showes a sandwich structure during the observation period. This is different from our previous understanding and suggests that the strait exchange may have different modes varying with the forcing condition.
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