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中国东部地区秋末冬初大雾多发的异常环流特征及成因

桑小卓 陈圣劼 刘端阳 张然 王博妮 周文君

气象学报2025,Vol.83Issue(2):240-256,17.
气象学报2025,Vol.83Issue(2):240-256,17.DOI:10.11676/qxxb2025.20240071

中国东部地区秋末冬初大雾多发的异常环流特征及成因

Circulation anomalies and formation mechanisms for late autumn and early winter fog occurrences over eastern China

桑小卓 1陈圣劼 2刘端阳 3张然 3王博妮 1周文君2

作者信息

  • 1. 江苏省气象服务中心,南京,210041
  • 2. 江苏省气象台,南京,210041
  • 3. 南京气象科技创新研究院 中国气象局交通气象重点实验室,南京 210041
  • 折叠

摘要

Abstract

Daily observations collected at meteorological gauge stations in eastern China and ERA5 reanalysis data for the period of 1960-2022 are utilized to investigate the key circulation in late autumn and early winter fog days in eastern China and its formation mechanisms based on statistical analysis and dynamical diagnosis.Results show that when fog days are prevalent in eastern China during late autumn and early winter,a significant positive geopotential height anomaly occurs in the middle and upper troposphere along the East Asian coast and the East Asian trough weakens,which is not conducive to the eastward and southward movement of cold air.There are an anticyclonic circulation anomaly in the lower troposphere to the east of 120°E and a cyclonic circulation anomaly to the west accompanied with significant southerly wind anomalies along the East Asian coast,corresponding to weakened East Asian winter monsoon,reduced sea level pressure gradient,and weak near-surface wind speed.The warm advection caused by the anomalous southerly winds is the dominant factor that affects the atmospheric stability,promoting the formation and maintenance of temperature inversion layers.Moreover,the southerly wind anomalies are also favorable for the northward transport of water vapor and cause moisture flux convergence in eastern China,providing a sufficient water vapor condition for the formation of fog.The large-scale circulation anomalies associated with fog days in eastern China are synergistically affected by El Niño and mid-and high-latitude wave trains.El Niño is conducive to anomalous low-level anticyclone in the western North Pacific,and the mid-and high-latitude Rossby wave trains triggered by the negative wave source in central Europe cause high pressure anomalies in the middle and upper troposphere along the East Asian coast.The results of this study enhance our understanding of the formation mechanisms for late autumn and early winter fog days in eastern China,and lay a foundation for subseasonal and seasonal fog prediction.

关键词

大雾多发/环流异常/厄尔尼诺/中高纬波列/秋末冬初/中国东部

Key words

Frequent fog/Anomalous circulation/El Niño/Mid-and high-latitude Rossby wave trains/Late autumn and early winter/Eastern China

分类

天文与地球科学

引用本文复制引用

桑小卓,陈圣劼,刘端阳,张然,王博妮,周文君..中国东部地区秋末冬初大雾多发的异常环流特征及成因[J].气象学报,2025,83(2):240-256,17.

基金项目

江苏省科协青年科技人才托举工程(TJ-2022-053)、江苏省自然科学基金项目(BK20231396). (TJ-2022-053)

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