赤道洋流（equatorial current）指在信风的影响下在赤道附近海水自东向西大规模移动形成的巨大洋流系。赤道洋流由三大洋流组成：在信风影响之下形成向西流动的南赤道洋流和北赤道洋流；在信风带之间的最低风压带内形成的向东流动的赤道逆流；以及赤道表层海水之下向东流动的赤道潜流。
... energy current 有功电流,有效电流 equatorial current 赤道洋流 excess current 过剩电流 ...
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... Equatorial latent current 赤道潜流 equatorial drift current 赤道洋流 south equatorial drift current 南赤道漂流 ...
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南赤道洋流 South Equatorial Current
北赤道洋流 north equatorial current
印度洋赤道洋流 Indian Ocean equatorial current
地赤道洋流 south equatorial current
太平洋赤道潜流 [海洋] Pacific equatorial undercurrent
赤道海洋流体动力学 [海洋] hydrodynamics of equatorial ocean
大西洋赤道潜流 [海洋] Atlantic Equatorial Undercurrent
太平洋北赤道流 [海洋] Pacific North Equatorial Current
印度洋赤道潜流 Indian Equatorial Undercurrent
Ocean current’s change is characterized by enhancement of equatorial current and equatorial counter current, therein the latter results in SST’s rising in eastern equatorial ocean where SST is lower originally.
洋流的变化主要表现为南北赤道洋流和赤道逆流(主要是太平洋)的增强,后者使赤道大洋中东部的海温有所升高,改善了该地区海温偏低的现象。
参考来源 - NCC/IAP T63海气耦合模式云辐射参数化方案的改进及其在气候模拟中的应用·2,447,543篇论文数据，部分数据来源于NoteExpress
能模拟出低频运动并有助于建立和维持赤道洋流系统的波动有着特殊的意义。
Of particular interest are waves that simulate low-frequency motions and that help to establish and maintain the equatorial current system.
南赤道洋流无论哪个季节都穿过赤道，在赤道以北的南赤道洋流冬季比夏季强，而在赤道以南的南赤道洋流夏季比冬季强。
The South Equatorial Current which located in the north of the equator is stronger in winter than it is in summer, but the one in the Southern Hemisphere is strong in summer and weak in winter.
Stowe计划了一条航线将最初把两人带到北大西洋，从而能利用那里的海风和洋流，然后驶向赤道南部。
Stowe planned a course that initially will take them into the north Atlantic to take advantage of wind and currents, then head south of the Equator.
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