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Long‐term changes in the relationship between stratospheric circulation and East Asian winter monsoon

机译:平流层环流与东亚冬季风关系的长期变化

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Using two generations of reanalysis datasets from the National Center for Atmospheric Research ( NCAR ), European Centre for Medium‐Range Weather Forecasts ( ECMWF ), and Japan Meteorological Agency ( JMA ), we showed that on the interannual timescale the two leading modes of the East Asian winter monsoon ( EAWM ) are associated with tropospheric annular mode ( AM ) and stratospheric polar vortex ( SPV ), respectively. The relationship between AM and the first EAWM mode remained stable during 1958–2013, whereas that between SPV and the second EAWM mode increased suddenly since the late 1980s. The SPV ‐related circulation and planetary wave activities are intensified in the latter period. We suggested that this change might be caused by the global warming and ozone depletion.
机译:使用美国国家大气研究中心(NCAR),欧洲中距离天气预报中心(ECMWF)和日本气象厅(JMA)的两代再分析数据集,我们发现,在年际时标上,两种主导模式东亚冬季风(EAWM)分别与对流层环形模式(AM)和平流层极涡(SPV)相关。在1958年至2013年期间,AM与第一种EAWM模式之间的关系保持稳定,而SPV与第二种EAWM模式之间的关系自1980年代后期以来突然增加。在后期,与SPV有关的环流和行星波活动加剧。我们建议这种变化可能是由于全球变暖和臭氧消耗引起的。

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