我国近海(指黄、东海部分,下同),是一个水深约在100米以内,海岸曲折,外有洋流入侵,内多入海径流,而且季节风盛行的浅海。同时,水文分布情况,具有明显的季节变化,最显著的特点是:在降温期内,海水几呈垂直均匀状态;而在增温期间,则出现明显的层化现象。 研究在这种真实条件下的复杂的海流情况,显然是十分困难的。现有的海流理论, China’s offshore (referring to the Yellow Sea, the East China Sea part, the same below) is a shallow water depth of about 100 meters, the coast twists and turns, the influx of ocean currents, the more into the sea runoff, and the prevalence of seasonal wind shallow sea. At the same time, the distribution of hydrology has obvious seasonal changes. The most notable feature is that during the cooling period, the seawater is almost vertically vertical, while during the warming period, obvious stratification occurs. It is obviously very difficult to study the complicated current situation under such real conditions. The current ocean current theory,