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气象:2006,32(3):49-55
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2005年3月一次寒潮天气过程的诊断分析
(1.江西省气象台,南昌 330046;2.国家气象中心)
Diagnosis of a Cold Wave Weather Event in March 2005
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投稿时间:2005-12-15    修订日期:2006-01-13
中文摘要: 利用NECP1°×1°的6小时分析资料和常规观测等资料,对2005年3月10~13日一次全国性寒潮天气过程的环流背景、影响天气系统及成因进行了分析。结果表明:这次寒潮及寒潮天气主要成因是(1)西欧上空500hPa强暖平流致使在西伯利亚地区形成阻塞高压,建立横槽,横槽北侧的东北气流引导超极地冷空气和西路冷空气合并加强;形成了异常强的冷高压、锋区、冷温度中心和冷温度平流。(2)两个短波槽东移侵入阻塞高压,使得横槽两次建立和转为竖槽,导致强冷空气大举南侵。(3)寒潮带来大范围强降温、700hPa西南急流与冷空气
Abstract:Based on NCEP 1°×1° 6h interval reanalyzed data and daily observation data, the circulation background, synoptic weather systems and the formation mechanism of the cold wave event covering the whole country on 10—13 March 2005 are discussed. The results show that the formation mechanisms of the event are as follows. (1) The strong warm advection of 500hPa over the west Europe led to a blocking high created in Siberia area, and a zonal though, the north-east stream in the north edge of the though led to super polar cold air and the cold air from west together and got to strengthen, and then the abnormally strong cold high, front zone, cold temperature center and cold temperature advection appear. (2) The two short-wave troughs moving eastwards intruded into the blocking high, which made the zonal trough created and became a meridianal one for two times, resulting in the strong cold air greatly moved into southern area. (3) The three conditions, involving the temperature sharp drop, the convergence of west-south jet stream and the cold air stream at 700hPa, and the vertical temperature distribution of the area below 0℃ above 1000hPa, provided the main factors of dynamics, moisture and condensation for severer snow in southern China.
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引用文本:
许爱华,乔林,詹丰兴,牛星球,2006.2005年3月一次寒潮天气过程的诊断分析[J].气象,32(3):49-55.
,2006.Diagnosis of a Cold Wave Weather Event in March 2005[J].Meteor Mon,32(3):49-55.