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中国农学通报 ›› 2010, Vol. 26 ›› Issue (24): 307-312.

所属专题: 农业气象

• 资源 环境 生态 土壤 气象 • 上一篇    下一篇

石家庄地区一次西风槽系统下云物理特征的分析

孙玉稳 孙 霞 姜 岩 齐作辉   

  • 收稿日期:2010-05-05 修回日期:2010-08-26 出版日期:2010-12-20 发布日期:2010-12-20
  • 基金资助:

    科技部公益性行业(气象)科研专项

the Cloud Physical Feature Affected by an Westerly Trough in Shijiazhuang

  • Received:2010-05-05 Revised:2010-08-26 Online:2010-12-20 Published:2010-12-20

摘要:

摘 要河北省小麦主产区中南部地区春季最多的降雨系统为西风槽系统,为研究西风槽系统影响下的云物理结构特征,本文对2006年5月8日至9日一次西风槽过程,石家庄地区云物理特征进行分析。分析得到:本次西风槽降水云层薄并夹有干层,观测所得的云中含水量最大为0.30g/m3,平均含水量较低;石家庄地区处于西风槽底部,不利于降水的形成;另外,由于云中含水量较低和干层的存在使云滴和雨滴的蒸发,导致石家庄市降水只为1mm。

关键词: 霍奎耶羊驼, 霍奎耶羊驼, 毛囊, 兴盛期, 结构

Abstract:

Abstract The westerly trough is the most precipitation system in central and southern areas of Hebei province, where is the major wheat production area. In order to study the feature of cloud physical structure affected by westerly trough, we analyzed an westerly trough procedure from May 8 to 9 in 2006. It was concluded that: this westerly trough precipitation has thin cloud with dry layer. Observations indicated that the mean moisture content in the cloud is low, with a maximum value of 0.30 g/m3; Shijiazhuang is in the bottom of westerly trough. It is the disadvantage for precipitation; in addition, the low moisture content and the dry layer in the cloud made the cloud droplet and raindrop evaporate, leading the low precipitation of 1 mm in Shijiazhuang.