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Subsurface currents : ウィキペディア英語版 | Subsurface currents
A subsurface current is an oceanic current that runs beneath surface currents.〔(【引用サイトリンク】work=Glossary of Meteorology )〕 Examples include the Equatorial Undercurrents of the Pacific, Atlantic, and Indian Oceans, the California Undercurrent,〔Pierce, S. D. et al (2000). "[〕 and the Agulhas Undercurrent, the deep thermohaline circulation in the Atlantic, and bottom gravity currents near Antarctica. The forcing mechanisms vary for these different types of subsurface currents. ==Density current== The most common of these is the density current, epitomized by the Thermohaline current. The density current works on a basic principle: the denser water sinks to the bottom, separating from the less dense water, and causing an opposite reaction from it. There are numerous factors controlling density.
抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)』 ■ウィキペディアで「Subsurface currents」の詳細全文を読む
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