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2021年11月7-9日辽宁省极端雨雪天气分析

高清源 金巍 高清泉 徐庆喆 田璐 刘冬霞 韩国敬

气象与环境学报2024,Vol.40Issue(2):1-8,8.
气象与环境学报2024,Vol.40Issue(2):1-8,8.DOI:10.3969/j.issn.1673-503X.2024.02.001

2021年11月7-9日辽宁省极端雨雪天气分析

Diagnostic analysis of the extreme rain-snow process in Liaoning province from November 7-9,2021

高清源 1金巍 2高清泉 3徐庆喆 1田璐 1刘冬霞 4韩国敬1

作者信息

  • 1. 鞍山市气象局,辽宁鞍山 114000
  • 2. 辽宁省气象台,辽宁沈阳 110166||中国科学院空间天气学国家重点实验室,北京 100190
  • 3. 廊坊市气象局,河北廊坊 065000
  • 4. 中国科学院大气物理研究所中层大气与全球环境重点实验室,北京 100029
  • 折叠

摘要

Abstract

The conventional meteorological observation data,artificially enhanced observation data and NCEP/NCAR(the National Centers for Environmental Prediction and the National Center for Atmospheric Research)grid data were used to analyze the extreme rain and snow weather in Liaoning province from November 7-9,2021.The results show that the Northeast China Cold Vortex(NCCV)and the surface cyclone are the main influence systems of the extreme rain and snow weather.The convergence of the middle and lower troposphere,the diver-gence of the upper troposphere and the convergence of the strong cold and warm air flow are the main causes of the extreme rain and snow weather.The coupling of the high and low level jet and the high level divergence suc-tion,together with the dynamic lifting effect of the NCCV,the warm and wet low level jet climb along the cold pad,which further strengthen the upward motion.The warm moist jet provides abundant water vapor conditions for the extreme rain and snow weather,and the strengthening of the warm moist jet corresponds to the strengthening of water vapor convergence,combined with the dynamic lifting effect of the low-level cold pad and the NCCV,and the ground convergence line distributes along the terrain,which triggers the extreme heavy snow weather.Terrain blocking leads to the accumulation of cold air on the ground to form cold air cushion,which is an important reason for extreme snowfall.The difference of temperature stratification is the main reason for the difference of rain and snow phase between Anshan and Xiuyan.The low layer cold air cushion with the characteristics of freezing layer provides favorable temperature stratification conditions for the extreme snowstorm in Anshan.The melting layer thickness and ground temperature are the key factors for the occurrence of freezing rain in Xiuyan.

关键词

东北冷涡/暖湿急流/冷垫/温度层结

Key words

Northeast China Cold Vortex(NCCV)/Warm moist jet stream/Cold air cushion/Temperature stratifi-cation

分类

天文与地球科学

引用本文复制引用

高清源,金巍,高清泉,徐庆喆,田璐,刘冬霞,韩国敬..2021年11月7-9日辽宁省极端雨雪天气分析[J].气象与环境学报,2024,40(2):1-8,8.

基金项目

国家自然科学基金面上项目(41875007)、中国科学院国家空间科学中心空间天气学国家重点实验室"地磁活动与大气环流变化的关联影响"项目和辽宁省气象局人才计划科技活动资助项目(RC202201)共同资助. (41875007)

气象与环境学报

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