Transports and pathways of the tropical AMOC return flow from Argo data and s...
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The upper-ocean circulation of the tropical Atlantic is a complex superposition of thermohaline and wind-driven flow components. The resulting zonally- and vertically-integrated...
热带大西洋上层海洋环流,由热盐(thermohaline)驱动的流动分量与风驱流动分量复杂叠加而成。由此得到的纬向积分与垂直积分……



