The Impact of Tropical Sea Surface Temperature on the Arctic Stratospheric Polar Vortex Trend

IF 3.5 3区 地球科学 Q2 METEOROLOGY & ATMOSPHERIC SCIENCES
Cuijuan Sui, Alexey Yu Karpechko, Lejiang Yu, Licheng Feng, Shan Liu
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Abstract

The changes in the Arctic stratospheric polar vortex are influenced by various factors and exert impacts on both the weather and climate of the troposphere and the surface. In this study, we analysed the trends of the stratospheric polar vortex using the self-organising map (SOM) method. There is a decreasing trend in the occurrence of strong polar vortices, while there is an increasing trend in the occurrence of weak polar vortices. The analysis revealed that nine nodes (3 × 3) of SOMs can explain approximately one-third (the trend contribution ratio is 33.4%) of the significant increase in the geopotential height field, in which two nodes (Nodes 3 and 7) amount to approximately three-quarters (25.23%) of the total contribution (33.4%). Significantly positive sea surface temperature (SST) anomalies in the tropical western Pacific and the southwestern Pacific Ocean associated with Node 3 enhanced convective activity in these areas, resulting in negative Rossby wave sources (RWS) and divergent winds, triggering a Rossby wave train. This wave train generates positive geopotential height anomalies over the Arctic Ocean in the stratosphere, which helps weaken the Arctic polar vortex. A wave train excited by suppressed convective activity in the tropical West Pacific and South China Sea related to Node 7 propagates northeastward along a similar path to middle and high latitudes. However, this wave train induces geopotential height anomalies opposite in sign over the Arctic Ocean, which favours the strengthening of the polar vortex. The EP flux in the high-latitude lower stratosphere associated with the two above wave trains can explain the Arctic polar vortex anomalies. Our results show that the influence of SST in the warm pool region on the stratospheric polar vortex is greater than in other ocean regions.

热带海表温度对北极平流层极涡趋势的影响
北极平流层极涡的变化受多种因素的影响,对对流层和地面的天气气候都有影响。本文采用自组织图(SOM)方法分析了平流层极涡的变化趋势。强极涡的出现有减少的趋势,弱极涡的出现有增加的趋势。分析表明,9个节点(3 × 3)的som可以解释约1 / 3的位势高度场显著增加(趋势贡献率为33.4%),其中2个节点(节点3和节点7)约占总贡献(33.4%)的3 / 4(25.23%)。与节点3相关的热带西太平洋和西南太平洋显著的海温正异常增强了这些地区的对流活动,导致负罗斯比波源(RWS)和辐散风,触发了罗斯比波列。这种波列产生平流层中北冰洋上空的正位势高度异常,这有助于削弱北极极地涡旋。与节点7有关的热带西太平洋和南海受抑制对流活动激发的波列沿相似路径向东北方向传播至中高纬度地区。然而,这一波列在北冰洋上空引起位势高度异常,这有利于极地涡旋的加强。与上述两个波列相关的高纬平流层低层EP通量可以解释北极极涡异常。结果表明,暖池区海温对平流层极涡的影响大于其他海洋区。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
International Journal of Climatology
International Journal of Climatology 地学-气象与大气科学
CiteScore
7.50
自引率
7.70%
发文量
417
审稿时长
4 months
期刊介绍: The International Journal of Climatology aims to span the well established but rapidly growing field of climatology, through the publication of research papers, short communications, major reviews of progress and reviews of new books and reports in the area of climate science. The Journal’s main role is to stimulate and report research in climatology, from the expansive fields of the atmospheric, biophysical, engineering and social sciences. Coverage includes: Climate system science; Local to global scale climate observations and modelling; Seasonal to interannual climate prediction; Climatic variability and climate change; Synoptic, dynamic and urban climatology, hydroclimatology, human bioclimatology, ecoclimatology, dendroclimatology, palaeoclimatology, marine climatology and atmosphere-ocean interactions; Application of climatological knowledge to environmental assessment and management and economic production; Climate and society interactions
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