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Estimates of global ocean volume transports during 1960 through 2001

机译:1960年至2001年全球海洋运输量的估计

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摘要

An estimate of global time-varying ocean volume transports is provided for the period 1960-2001 as it results from the German ECCO (GECCO) synthesis. Results confirm previously discussed mean-state ocean circulation systems, encompassing an upper meridional cell in the Atlantic with sinking in the North Atlantic connected to a lower meridional cell with sinking around Antarctica in the Pacific and Atlantic. Decadal to interdecadal variability as well as long-term trends of global ocean transport, analyzed over the course of the 42 years, appear as a reorganization of time-mean circulation structures, including the layer transports in the Antarctic Circumpolar Current (ACC) and the circulation involving the Indo-Pacific exchange.
机译:由于德国ECCO(GECCO)的综合结果,因此提供了1960-2001年期间全球时变海洋运输量的估计值。结果证实了先前讨论的平均状态海洋环流系统,包括大西洋的一个上子午线细胞和北大西洋的下沉细胞,而下个子午线细胞则沉没在太平洋和大西洋的南极周围。在过去的42年中分析了年代际变化和全球海洋运输的长期趋势,这是时均环流结构的重组,包括南极绕极洋流(ACC)和南极环流涉及印度太平洋交换的流通。

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