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运用卫星跟踪漂移浮标资料分析南海表层海流 ,研究了有关海域的表层海流特征。结果表明 ,秋、冬季入侵南海的黑潮水有一小部分沿台湾南岸折回黑潮主干 ,并有时在台湾西南外海形成反气旋涡旋 ,其余大部分黑潮水西行进入南海内部。吕宋岛西部沿岸流始于 1 3°N以南 ,沿菲律宾西海岸北上抵达吕宋岛西北角 ,与黑潮水混合后西行
Using satellite tracking drift buoy data to analyze the surface currents in the South China Sea, the characteristics of the surface currents in the relevant sea areas are studied. The results showed that a small part of the Kuroshio water intruded into the South China Sea in autumn and winter turned back the main Kuroshio along the south bank of Taiwan. Sometimes it formed an anti-cyclonic vortex off the southwest coast of Taiwan. Most of the Kuroshio reached the interior of the South China Sea. The western Luzon coast flows south of 13 ° N and reaches the northwestern tip of Luzon Island along the west coast of the Philippines northward and westbound after mixing with Kuroshio