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东亚冬季气温异常冷暖反转模态的非对称特征及其维持机制

李乔 刘伯奇

大气科学2025,Vol.49Issue(6):1691-1710,20.
大气科学2025,Vol.49Issue(6):1691-1710,20.DOI:10.3878/j.issn.1006-9895.2501.24041

东亚冬季气温异常冷暖反转模态的非对称特征及其维持机制

Asymmetric Characteristics and Maintenance Mechanisms of the East Asian Winter Temperature Anomaly Reversal Mode

李乔 1刘伯奇1

作者信息

  • 1. 中国气象科学研究院灾害天气科学与技术全国重点实验室,北京 100081
  • 折叠

摘要

Abstract

The reversal of temperature anomalies from warm to cold and vice versa in the East Asian region is a significant climatic phenomenon occurring during the winter season under the context of global warming.Compared to the variability of seasonal-mean winter temperature anomalies,the climate prediction uncertainty for the reversal phenomenon is greater,and its adverse effects are more significant.In this study,seasonal empirical orthogonal decomposition and composite analysis were performed on atmospheric reanalysis data from the winters of 1980/81 to 2022/23 to investigate the interannual variability of the East Asian winter temperature anomaly reversal mode(TARM).The results indicate that although the different processes of the East Asian winter TARM are related to intraseasonal reversals of the Siberian High,the Eurasian teleconnection,and the Arctic vortex anomalies,the interannual variability of the"warm-to-cold"mode is significantly stronger than that of the"cold-to-warm"mode,suggesting a pronounced asymmetry in the interannual variability of TARM.In the"warm-to-cold"mode,the lower-level Siberian High strengthens over time:the positive phase of the East Atlantic-West Russia-like teleconnection in early winter shifts to a negative phase in late winter,leading to more active cold air.Conversely,in the"cold-to-warm"mode,the intensity of the winter Arctic vortex shifts from weak to strong,and subsequently,the Siberian High weakens,favoring the appearance of temperature anomalies that are cold in early winter and warm in late winter.Further analysis shows that the North Atlantic and tropical Indian Ocean sea surface temperature anomalies with La Niña are important factors influencing the"warm-to-cold"mode,while a reduction in the Barents-Kara sea ice in November acts as a precursor signal for the"cold-to-warm"mode.Therefore,the diversity of underlying atmospheric conditions is an important cause of the asymmetry of the East Asian winter TARM.Therefore,climate prediction for the East Asian winter TARM should consider the diversity of the underlying atmospheric conditions.

关键词

东亚冬季风/气温异常/冷暖季节内反转/年际变化/非对称性

Key words

East Asia winter monsoon/Air temperature anomaly/Subseasonal reversal between warm and cold anomalies/Interannual variability/Asymmetric features

分类

天文与地球科学

引用本文复制引用

李乔,刘伯奇..东亚冬季气温异常冷暖反转模态的非对称特征及其维持机制[J].大气科学,2025,49(6):1691-1710,20.

基金项目

国家自然科学基金项目U2242205、42375033,中国气象科学研究院科技发展基金项目2023KJ036,基本科研业务费项目2023Z018,气象能力提升联合研究专项24NLTSZ001 National Natural Science Foundation of China(Grants U2242205,42375033),Science&Technology Development Foundation of the Chinese Academy of Meteorological Sciences(CAMS)(Grant 2023KJ036),Basic Scientific Research and Operation Foundation of the CAMS(Grant 2023Z018),Joint Research Program for Enhancing Meteorological Capabilities(Grant 24NLTSZ001) (Grants U2242205,42375033)

大气科学

OA北大核心

1006-9895

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