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Anticorrelated multidecadal variations between surface and subsurface tropical North Atlantic

机译:热带北大西洋和地下热带之间反相关的年代际变化

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摘要

In this paper for the first time I show that the multidecadal variations of observed tropical North Atlantic ( TNA) sea surface temperature (SST) are strongly anticorrelated with those of the observed TNA subsurface ocean temperature, with long-term trends removed. I further show that the anticorrelated change between the TNA surface and subsurface temperature is a distinctive signature of the Atlantic meridional overturning circulation (AMOC) variations, using water-hosing experiments with the GFDL state-of-art coupled climate model (CM2.1). External radiative forced simulations with the same model do not provide a significant relationship between the TNA surface and subsurface temperature variations. The observed detrended multidecadal TNA subsurface temperature anomaly may be taken as a proxy for the AMOC variability. Various mechanisms proposed for the multidecadal TNA SST variations, which are crucial for multidecadal variations of Atlantic hurricane activities, should take into account the observed anticorrelation between the TNA surface and subsurface temperature variations.
机译:在本文中,我第一次表明,观测到的热带北大西洋(TNA)海表温度(SST)的年代际变化与观测到的TNA地下海洋温度的年代际变化强烈反相关,并且消除了长期趋势。我进一步证明,使用GFDL最先进的耦合气候模型(CM2.1)进行水套实验,TNA表面和地下温度之间的反相关变化是大西洋子午翻转循环(AMOC)变化的独特标志。 。具有相同模型的外部辐射强迫模拟在TNA表面和地下温度变化之间没有提供显着的关系。所观测到的去趋势的多年代际TNA地下温度异常可以作为AMOC变异的代理。对于大西洋飓风活动的多年代变化至关重要的多年代TNA SST变化建议的各种机制,都应考虑到TNA表面和地下温度变化之间观察到的反相关性。

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