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首页> 外文期刊>Geophysical Research Letters >Sensitivity of northern hemisphere surface climate to simulation of the stratospheric polar vortex - art. no. 1627
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Sensitivity of northern hemisphere surface climate to simulation of the stratospheric polar vortex - art. no. 1627

机译:北半球表面气候对平流层极涡模拟的敏感性-艺术没有。 1627

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摘要

1] A sensitivity experiment has been performed with a stratosphere-resolving GCM where the mean state and variability of the stratosphere have been altered. It is shown that this has a significant effect on the mean and variability of wintertime northern hemisphere surface climate. In particular it is shown that the stratosphere strongly contributes to the persistence of the surface Arctic Oscillation at lags of 10 - 25 days. This confirms the importance of the stratosphere on surface climate that has been inferred by recent studies examining the Arctic Oscillation in reanalysis datasets. [References: 14
机译:1]用平流层解析GCM进行了敏感性实验,其中平流层的平均状态和变异性已经改变。结果表明,这对冬季北半球冬季表面气候的平均值和变异性有重大影响。特别是,平流层在10到25天的滞后强烈促进了表面北极涛动的持续性。这证实了平流层对地表气候的重要性,这是根据最近在重新分析数据集中检查北极涛动的研究得出的。 [参考:14

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