Yellow Sea | Sea, Asia - Britannica

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Hydrology

The warm current of the Yellow Sea is a part of the Tsushima Current, which diverges near the western part of the Japanese island of Kyushu and flows at less than 0.5 mile (0.8 km) per hour northward into the middle of the sea. Along the continental coasts, southward-flowing currents prevail, which strengthen markedly in the winter monsoon period, when the water is cold, turbid, and of low salinity.

The tidal range is high (13 to 26 feet [4 to 8 metres]) along the shallower west coast of the Korean peninsula, with a maximum spring tide of almost 27 feet (8.2 metres). Along the coasts of China, it amounts to about 3 to 10 feet (0.9 to 3 metres), except around the Bo Hai, where it is somewhat higher. In the Yellow Sea the tides are semidiurnal (i.e., they rise twice daily). The tidal system rotates in a counterclockwise direction. The speed of the tidal current is generally less than 1 mile (1.6 km) per hour in the middle of the sea, but, near the coasts and in the straits and channels, stronger currents of more than 3.5 miles (5.6 km) per hour are recorded.

The innermost coastal sections of the Bo Hai freeze in winter, and drift ice and ice fields hinder navigation in parts of the Yellow Sea. Surface temperature ranges from freezing level in winter in the Bo Hai to summer temperatures of 72 to 82 °F (22 to 28 °C) in the shallower parts. In winter the temperature and salinity in the sea are homogeneous from surface to bottom. In spring and summer the upper layer is warmed and diluted by the fresh water from rivers, while the deeper water remains cold and saline. This deep layer of cold water stagnates and moves slowly south in summer. Around this mass of water, especially at its southern tip, commercial bottom-dwelling fishes are found. The dominant salinity in the region is relatively low: in the Bo Hai it is 30 to 31 parts per thousand, while in the Yellow Sea proper it is 31 to 33 parts per thousand. In the southwest monsoon season (June to August) the increased rainfall and runoff cause a further reduction in salinity in the upper layer.

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