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单词 North Equatorial Current
释义

North Equatorial Current

中文百科

北赤道暖流

世界洋流概要。

北赤道暖流(英语:North Equatorial Current),或称为北赤道洋流,为一个显著的太平洋及大西洋洋流,在北纬10度至20度由东向西流。北赤道暖流为亚热带环流(Subtropical Gyre)的南部组成部分。虽然其名为北赤道暖流,但北赤道暖流并不与赤道有连接。在两个海洋中,北赤道暖流因为向东流的赤道逆流阻隔而与赤道循环分开。在两个海洋的西行水流为南赤道洋流的一部分。

英语百科

North Equatorial Current 北赤道暖流

The North Equatorial Current is a significant Pacific and Atlantic Ocean current that flows east-to-west between about 10° north and 20° north. It is the southern side of a clockwise subtropical gyre. Despite its name, the North Equatorial Current is not connected to the equator. In both oceans, it is separated from the equatorial circulation by the Equatorial Countercurrent (also known as the North Equatorial Countercurrent), which flows eastward. The westward surface flow at the equator in both oceans is part of the South Equatorial Current.

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更新时间:2025/6/21 5:00:57