北方农业学报 ›› 2015, Vol. 43 ›› Issue (3): 100-100.

• • 上一篇    下一篇

呼和浩特市一次降雪天气分析

杨彩云   

  1. 呼和浩特市气象局,内蒙古呼和浩特010020
  • 出版日期:2015-06-20 发布日期:2015-06-20
  • 通讯作者: 杨彩云
  • 作者简介:杨彩云(1980-),女,内蒙古呼和浩特人,工程师,主要从事天气气候预测预报工作。

Analysis of a snowfall processes occurred in Hohhot

YANG Caiyun (Hohhot meteorol.gical bureau,Hohhot 010020,China)   

  • Online:2015-06-20 Published:2015-06-20

摘要: 应用常规地面观测资料、FNL资料(水平分辨率为1.0°×1.0°,时间间隔为6 h),从环流形势、物理量场等方面对2014年2月18-19日呼和浩特市发生的一次降雪天气过程进行了分析。结果表明:高空短波槽东移,中低层风场存在明显切变线以及地面倒槽相配合,为该次降雪提供了有利的环流形势;高层辐散、低层辐合以及较强的上升运动为水汽的垂直输送提供了有利的动力条件;由南向北延伸至呼和浩特地区的暖湿空气为该次降雪积蓄了大量的不稳定能量。

Abstract: Based on the surface observation data and FNL data (horizontal resolution was 1.0°×1.0°,time interval was 6h),a snowfall processes occurred on February 18 and 19 2014 in Hohhot was analyzed in the aspect of circulation pattern, physical quantity field and others.The results showed that the synergistic effect of high altitude short wave trough moving to east,the shear line existing in middle and low level wind field and the ground inverse trough provided a favorable circulation pattern for the snowfall processes.The upper level divergence,low level convergence and strong ascending motion provided favorable dynamic condition for the vertical transport of water vapor.Furthermore, the warm moist air extending from south to north to Hohhot accumulate an amount of instability energy for the snowfall.

中图分类号: 

  • P458.121