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中国冬季地表温度主模态的月际变化特征及其与大气环流模态的联系

王远恒 姚永红 吴其冈

大气科学学报2025,Vol.48Issue(6):926-940,15.
大气科学学报2025,Vol.48Issue(6):926-940,15.DOI:10.13878/j.cnki.dqkxxb.20240430002

中国冬季地表温度主模态的月际变化特征及其与大气环流模态的联系

Monthly variability of the leading mode of winter surface air temperature in China and its relationships with the Northern Hemisphere teleconnection patterns

王远恒 1姚永红 1吴其冈2

作者信息

  • 1. 南京大学大气科学学院,江苏南京 210023
  • 2. 复旦大学大气与海洋科学系/大气科学研究院,上海 200438
  • 折叠

摘要

Abstract

In recent decades,inter-monthly variability of winter surface air temperature(SAT)in East Asia has become increasingly pronounced,often manifesting as sharp transitions between extreme cold and extreme warm events across different months or within different stages of winter.In China,SAT exhibits distinct month-to-month fluctuations,with some winters beginning anomalously warm and ending unusually cold,or vice versa.Previous studies have suggested that these fluctuations are influenced by atmospheric circulation anomalies and modulated by extratropical teleconnections in the mid-high latitudes.However,the specific teleconnection that exert dominant influence,as well as their relative roles,remain unclear. This study investigates the spatial and temporal characteristics of inter-monthly SAT anomalies in China and investigates the impacts of Eurasian mid-high latitude teleconnection patterns on SAT variability during December-January-February(DJF)over the period 1979-2020.The leading empirical orthogonal function mode(EOF1)of monthly SAT anomalies reveals a pan-China variability pattern,characterized by two distinct types:1)uniform anomalies of the same sign across DJF,and 2)anomalies of opposite sign between early winter(De-cember)and late winter(next January-February).Together,these two types account for approximately 50%of the total EOF1 variance. Analysis shows that the two types are associated with markedly different atmospheric circulation anomalies.Opposite-sign anomalies between early and late winter are primarily linked to the Polar-Eurasia(POL),East At-lantic(EA),and Eurasian(EU)patterns,while uniform anomalies across DJF are more strongly associated with the Arctic Oscillation(AO),POL,Scandinavian(SCA),western Pacific(WP),and EU patterns.These teleconnection anomalies alter the location and intensity of the Siberian high,thereby exerting significant control over inter-monthly SAT variability. The results highlight the dominant role of anomalous teleconnection patterns on monthly timescales in shaping the leading mode(EOF1)of winter SAT variability in China.This study provides new insights into the mechanisms driving inter-monthly temperature fluctuations,with implications for seasonal climate prediction.

关键词

自然正交函数/冬季地面气温/月际变化/遥相关型/西伯利亚高压

Key words

empirical orthogonal function/winter surface air temperature/monthly variability/teleconnection pattern/Siberia high

引用本文复制引用

王远恒,姚永红,吴其冈..中国冬季地表温度主模态的月际变化特征及其与大气环流模态的联系[J].大气科学学报,2025,48(6):926-940,15.

基金项目

福建省灾害天气重点实验室开放课题(2022KFKT01) (2022KFKT01)

国家自然科学基金项目(42375031) (42375031)

大气科学学报

OA北大核心

1674-7097

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