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根据中、日合作黑潮调查研究期间（1987－1993年）在九州西侧海域获得的水文资料，计算了129°E断面的地转流速和流量。着重提出129°E断面北侧存在一支较稳定的西向流；分析这支西向流的去向，指出它是向对马暖流输送黑潮水的重要途径；给出了这支西向流及黑潮通过该断面的流速、流轴、流幅及流量的变化特征。
Based on the hydrological data obtained from the western waters of Kyushu during the Sino-Japanese Cooperative Kuroshio survey (1987-1993), the geostrophic velocity and flow rate at the 129 ° E section were calculated. It is emphasized that there is a relatively stable westward stream on the north side of 129 ° E section. By analyzing the direction of this westward stream, it is pointed out that it is an important way to deliver Kuroshio water to the warmth of the Ma. The westward flow and the Kuroshio are given The section of the flow velocity, flow axis, flow rate and flow characteristics of changes.