J4 ›› 2004, Vol. 22 ›› Issue (1): 44-48.

• 论文 • 上一篇    下一篇

一次连续性冰雹天气过程的诊断分析

王王进1董安祥2沈治广1   

  1. 1.甘肃省庆阳市气象局,甘肃 西峰 745000;2.中国气象局兰州干旱气象研究所,甘肃 兰州 730020
  • 收稿日期:2004-02-06 修回日期:2004-03-17 出版日期:2004-03-30 发布日期:2004-03-30
  • 作者简介:王王进(1967—),男,甘肃省庆阳市人,工程师,从事天气预报工作.E-mail:qyqxjwangjin@sohu.com.
  • 基金资助:

    科技部2002年社会公益研究项目“西北地区人工防雹消雹技术”的资助

The Diagnostic Analysis of a Continuous Hail Process

WANGJin1,DONGAn-xiang2,SHENZhi-guang1   

  1. 1.Qingyang Meteorological Bureau,Gansu Xifeng 745000,China;2.Institute of Arid Meteorology,CMA,Lanzhou 730020,China
  • Received:2004-02-06 Revised:2004-03-17 Online:2004-03-30 Published:2004-03-30

摘要:

对2000年秋季发生在甘肃庆阳的一次连续性冰雹天气过程进行了诊断分析。结果表明:这次冰雹天气过程是由于低层大气能量不断积累、低空切变线触发不稳定能量释放而产生的。冰雹出现在中低层对流不稳定和低层暖平流、高层冷平流以及低层辐合、高层辐散的上升运动区。冰雹落区与高低空温度平流和总温度平流的分布有着较好的对应关系。

关键词: 冰雹, 天气形势, 热力条件, 动力条件

Abstract:

In this paper,a continuous hail process,which occurred at Qingyang in Gansuprovince in fall in 2000,was diagnosed.The results showed that the process was happened by the reasons of atmosphere energy accumulating continuously and unstable energy releasing touched of by shear line in lower level.Hail occurred in the ascending motion area which had convective instability at middle -lower level,warm advection at lower level,cold advection at higher level,convergence at lower level and divergence at higher level.The hail area was correlated well to the distribution of temperature advection.

Key words: influencing system, thermal condition, dynamic condition

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