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首页> 外文期刊>Journal of Physical Oceanography >Localization of Multidecadal Variability. Part Ⅰ: Cross-Equatorial Transport and Interbasin Exchange
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Localization of Multidecadal Variability. Part Ⅰ: Cross-Equatorial Transport and Interbasin Exchange

机译:多年代变率的本地化。第一部分:跨赤道运输和跨流域交换

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摘要

Multidecadal SST variability is studied in idealized one- and two-ocean-basin configurations, using simulations with the Modular Ocean Model. The authors demonstrate that the multidecadal variability on the global "conveyor type" circulation is localized in the North Atlantic Ocean. Interbasin exchange processes determine the locations where regions of deep-water formation occur and induce a localization of SST multidecadal anomalies in the Atlantic. The physics of this localization is subsequently investigated by considering more equatorially symmetric background flows in two-basin and one-basin configurations. A cross-equatorial flow in the Atlantic induces the localization of the multidecadal variability in the North Atlantic. By using the mechanism of multidecadal variability as proposed in 2002 by Te Raa and Dijkstra in a single-hemispheric configuration, the physics of these localization processes can be explained.
机译:使用模块化海洋模型进行模拟,研究了理想化的一海盆和两海盆配置下的多年代际海表温度变异性。作者证明,全球“输送带类型”环流的年代际变化位于北大西洋。盆地之间的交换过程确定了深水形成区域的发生位置,并引起了大西洋SST年代际异常的局部化。随后,通过考虑两盆和一盆配置中更多的赤道对称背景流,研究了这种定位的物理原理。大西洋中的跨赤道流引起了北大西洋多年代际变率的局部化。通过使用Te Raa和Dijkstra在2002年提出的单半球构型的多年代际变化机制,可以解释这些定位过程的物理原理。

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