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一次暴雨与特大暴雪并存的华北强降水过程分析

杨晓亮 王咏青 杨敏 李江波 张叶 田雨润

气象Issue(12):1446-1454,9.
气象Issue(12):1446-1454,9.DOI:10.7519/j.issn.1000-0526.2014.12.003

一次暴雨与特大暴雪并存的华北强降水过程分析

Analysis on Severe Heavy Precipitation Event with Rainstorm and Large Blizzard in North China

杨晓亮 1王咏青 2杨敏 1李江波 3张叶 4田雨润4

作者信息

  • 1. 南京信息工程大学,南京 210044
  • 2. 河北省气象台,石家庄 050021
  • 3. 河北省防雷中心,石家庄 050021
  • 4. 河北省气象台,石家庄 050021
  • 折叠

摘要

Abstract

Based on conventional observations and NCEP 1°×1°reanalysis data,causes and precipitation type of the rain and snow weather process in North China during 3-4 November 2012 are analyzed.The results show that the deep low vortex and surface cyclone are the systems that directly impact the process. The southeast low-level j et transporting the abundant moisture from the eastern sea leads to the atmos-pheric precipitable water over the entire rain and snow storm area,exceeding the average of the month. The high-level divergence systems superimposed on the low-level convergence systems of the vortex and the cyclone provide a strong and lasting upward movement for the severe rain and snow storm.The heavy rain area and the blizzard region respectively stand for the convection instability stratification and the con-ditional symmetric instability stratification,and the frontogenesis favours the heavy snow storm.The en-vironmental conditions of the snowflake formation and growth,and the melting of the snowflakes falling are equally important in determining the precipitation type.The combinations of the two reasons men-tioned above ensure the emergence of snow on the ground surface.

关键词

暴雨雪/降水相态/条件性对称不稳定

Key words

rain and snow storm/precipitation type/conditional symmetric instability

分类

天文与地球科学

引用本文复制引用

杨晓亮,王咏青,杨敏,李江波,张叶,田雨润..一次暴雨与特大暴雪并存的华北强降水过程分析[J].气象,2014,(12):1446-1454,9.

基金项目

公益性行业(气象)科研专项(GYHY201206004)、河北省气象局重点项目(12ky34)和河北省气象局“强对流创新团队”共同资助 ()

气象

OA北大核心CSCDCSTPCD

1000-0526

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