中文摘要：

分析两个都基于风压力和海洋吸收数据集证明印度尼西亚的 Throughflow 和 Throughflow 从阶段的华南海(吕宋岛海峡) 的 interannual 可变性。风异例在赤道的太平洋强迫在建立这种阶段关系起一个重要作用。在 El Ni 期间 ? o 事件，西的风爆炸加强北赤道水流并且导致一向北方它的分叉点变。作为结果，在自台湾东面的菲律宾海流向日本的暖流和明达瑙岛水流之间的卷运输的分区被改变，与自台湾东面的菲律宾海流向日本的暖流运输减少，明达瑙岛水流增加了。undershooting/overshooting 现象发生在吕宋岛海峡和 Sulawesi 明达瑙岛经过，由这二水流的可变性引起了。水运输从对有自台湾东面的菲律宾海流向日本的暖流运输的华南海增加和平减少，并且到印度洋的从太平洋的运输减少，明达瑙岛当前的运输增加了。状况在 La Ni 期间被颠倒 ? 一。因此，海洋动态意思是深刻的学习在印度尼西亚的 Throughflow 和吕宋岛海峡 Throughflow 之间的 interannual 可变性关系。

英文摘要：

Analysis both based on the wind stress and ocean assimilation dataset shows that the interannual variability of the Indonesian Throughflow and the South China Sea （Luzon Strait） Throughflow is out of phase. Wind anomaly forcing in the equatorial Pacific plays an important role in setting up this phase relation. During El NiSo events, the westedy wind bursts intensify the Northern Equator Current and induce a northward shift of its bifurcation point. As a result, the partition of volume transport between the Kuroshio and the Mindanao Current is changed, with the Kuroshio transport decreased and the Mindanao Current increased. The undershooting/overshooting phenomena occur at the Luzon Strait and the Sulawesi-Mindanao passage, caused by variability of these two currents. Water transport from the Pacific to the South China Sea increases with the Kuroshio transport decreased, and transport from the Pacific to the Indian Ocean decreases with the Mindanao Current transport increased. The situation is reversed during La Nina. Therefore, the ocean dynamic meaning is profound to study the interannual variability relationship between the Indonesian Throughflow and the Luzon Strait Throughflow.