主办单位:中国气象局沈阳大气环境研究所
国际刊号:ISSN 1673-503X
国内刊号:CN 21-1531/P

气象与环境学报

• 论文 • 上一篇    下一篇

“2009.2”沈阳暴雪天气诊断与预报误差分析

梁红1;马福全1;李大为1;刘建国2;魏红3;方斌4   

  1. 1. 沈阳市气象局,辽宁 沈阳 110168;2.铁岭市气象局,辽宁 铁岭 112000;3. 辽宁省气象局, 辽宁 沈阳 110001;4. 辽宁省防雷技术服务中心,辽宁 沈阳 110016
  • 收稿日期:2010-03-03 修回日期:2010-07-19 出版日期:2010-08-29 发布日期:2010-08-29

Diagnostic analysis of heavy snow in February 2009 and its forecast error in Shenyang

LIANG Hong1;MA Fu-quan1;LI Da-wei1;LIU Jian-guo2;WEI Hong3;FANG Bin4   

  1. 1. Shenyang Meteorological Bureau, Shenyang 110168, China; 2. Tieling Meteorological Bureau, Tieling 112000, China; 3. Liaoning Provincial Meteorological Bureau, Shenyang 110001, China; 4. Liaoning Thunder Prevention Technology Center, Shenyang 110016, China
  • Received:2010-03-03 Revised:2010-07-19 Online:2010-08-29 Published:2010-08-29

摘要: 针对2009年2月12—13日沈阳暴雪过程,运用Micaps资料和自动站资料,分析了大尺度天气形势及相关物理量场。结果表明:500 hPa南北两支槽在辽宁的叠加和地面蒙古气旋及江淮气旋的合并是此次暴雪过程的主要成因。强降雪出现在850 hPa涡度和200 hPa散度大值区内,对流层中低层辐合、高层辐散为强降雪提供了有利的动力条件;低空急流为暴雪区水汽来源,亦为对流不稳定能量释放的触发源,暴雪区还具备上干冷下暖湿的热力不稳定条件;降水性质的转换与850 hPa的温度、温度平流和地面气温有直接联系;暴雪过程无论从量级,还是降水起止、雨转雪时间均预报得较为准确,但对降雪量和积雪深度估计不足。

关键词: 暴雪, 环流形势, 物理量, 诊断分析, 雨雪转换, 预报误差

Abstract: Based on MICAPS (meteorological information comprehensive analysis and process system) data and meteorological data from automatic stations, the synoptic situation and relative physical field of heavy snow on February 12-13, 2009 in Shenyang were analyzed. The results indicate that the stacking of south and north ladder troughs in 500 hPa and integration of ground Mongolia cyclone and Jianghuai cyclone are the main reasons forming the heavy snow. The heavy snow occurs in large vorticity area of 850 hPa and large divergence area of 200 hPa. The middle and lower convergence and upper divergence in troposphere provide favorable power for the heavy snow. The low-level jet plays not only the vapor source of heavy snow area, but also the trigger source of releasing convective instability energy. There is the thermodynamic instability with the cold and dry upper level and the warm and wet lower level in heavy snow area. The conversion between rain and snow are related with temperature of 850 hPa, temperature advection and ground temperature. The heavy snow intensity, starting and ending times of precipitation, starting time of rain to snow are predicted accurately, except the amount of snow and depth of snow cover.

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