| 一次冰雹天气过程分析 |
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| 引用本文： | 白惠星,王健.一次冰雹天气过程分析[J].新疆气象,2002,25(3):7-8. |
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| 作者姓名： | 白惠星 王健 |
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| 作者单位： | 新疆环境气象中心 新疆乌鲁木齐830002
(白惠星)，新疆环境气象中心 新疆乌鲁木齐830002(王健) |
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| 摘 要： | 对奎玛流域一次冰雹天气的分析表明，在巴尔喀什湖低槽加强东移的环流背景下，低层水汽辐合、抬升启动和层结不稳定有利于该地区强对流的发生、发展，中尺度强对流云团的形成、发展是产生这次冰雹天气的主要原因。
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| 关 键 词： | 天气过程分析 冰雹 强对流云团 水汽辐合 抬升 大气环流 热力条件 |
| 文章编号： | 1002-0799(2002)03-0007-02 |
| 修稿时间： | 2001年11月27 |
Analysis of a Hail Process |
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| BAI Hui -xing,WANG Jian.Analysis of a Hail Process[J].Bimonthly of Xinjiang Meteorology,2002,25(3):7-8. |
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| Authors: | BAI Hui -xing WANG Jian |
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| Abstract: | The analysis on a hail process in the KuiMa river basin shows that under the circulation background which the tr ough in the Baerkashi Lake was strengthen ed and went east and the low -level moisture convergence ,lifting -up acti on and unstable stratification were good for the str ong convection occuring and develop ing in the area,the middle -scale con vective clouds came into being and developed was the main cause of the hail process. |
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| Keywords: | the KuiMa river basin hail strong convective clouds |
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