吉林省春季降水性层状云基本结构及降水潜力的初步研究
CSTR:
作者:
作者单位:

作者简介:

通讯作者:

中图分类号:

P458

基金项目:

本文受国家科研院所社会公益研究专项基金项目(编号:2001DIB10084)资助


THE PRELIMINARY STUDY OF THE BASIC STRUCTURE OF PRECIPITATING STRATUS AND PRECIPITATION POTENTIAL IN SPRING IN JILIN PROVINCE
Author:
Affiliation:

Fund Project:

  • 摘要
  • |
  • 图/表
  • |
  • 访问统计
  • |
  • 参考文献
  • |
  • 相似文献
  • |
  • 引证文献
  • |
  • 资源附件
  • |
  • 文章评论
    摘要:

    2001年、2002年利用美国粒子测量系统(PMS)对吉林省5~7月降水性层状云在实施人工增雨作业的同时进行了科研探测,取得了一批资料,对这些资料进行计算后得到以下结论: (1)吉林省春季降水性层状云宏观结构主要分为三种云型即:Ns、As op-Sc op、Astra。 (2)不同云型其云中过冷水含量、云滴数密度不同,其中Ns云型的云中过冷水含量、云滴数密度最大,分别达到0.2737g/m^3、205.3个/L,其次是Asop-Sc op云层,其过冷水含量、云滴数密度分别为0.1693g/m^3、117.5个/L,过冷水含量、云滴数密度最小的云层结构为Astra,分别为0.1054 g/m^3、98.6个/L。 (3)云中过冷水含量与云底高度为负相关,与过冷层厚度为正相关. (4)三种云型的云中过冷水含量、云滴数密度距0℃层高度的分布基本一致:在距0℃层高度以上400-600m高度范围内过冷水含量、云滴数密度达最大,之后随着距0℃层高度的增加云中过冷水含量、云滴数密度迅速减小。 (5)吉林省春季降水性层状云的可播度为86%;三种云型的人工降水潜力有所不同,即:Ns云型潜力最大,达41.3%,其次是As op-Sc op云型潜力为28.4%,潜力最小的云型为As tra,为26.6%。

    Abstract:

    In 2001~2002,using American Particle Measure Systems (PMS) to make a scientific research during man-made rain enhancement operation in precipitating stratus in May~July in Jilin province,some data were obtained,after making a calculation to these data,the following conclusions were drawn:(1) the macro structure of precipitating stratus in spring in Jilin province is classified into three types : Ns,As op-Sc op and Astra. Different cloud types have different super-cooled water content and cloud droplet amount density,the super-cooled water content and cloud droplet amount density in the cloud of Ns type are the largest,they are respectively 0.2737 g/m3,205.3/L,the second is in the cloud layer of As op-Sc op,0.1693 g/m3,117.5/L,the smallest is in the cloud layer of As tra,0.1054 g/m3,98.6/L.(2)The super-cooled water content in the cloud has a negative correlation with the height of cloud base,and has a positive correlation with the thickness of super-cooled layer. (3)The super-cooled water content and cloud droplet amount density have a basically coincidence with the distribution of the distance to 0 ℃ layer height in these three types of clouds: super-cooled water content and the cloud droplet amount density are the largest in the range of 400~600 meters above 0 ℃ layer height,then super-cooled water content and the cloud droplet amount density reduce rapidly along with the increase of 0 ℃ layer height. (4)The seeding operation rate of precipitating stratus in spring in Jilin province is 86%,the rainfall enhancement potential of these three types of clouds are different,Ns is the largest,up to 41.3%,the second is As op-Sc op,about 28.4%,the smallest is As tra,26.6%.

    参考文献
    相似文献
    引证文献
引用本文

刘健,李茂仑,蒋彤,米长树,陈知新.吉林省春季降水性层状云基本结构及降水潜力的初步研究.气象科学,2005,(6):609-616 Liu Jian, Li Mao Lun, Jiang Tong, Mi Changshu, Chen Zhixin. THE PRELIMINARY STUDY OF THE BASIC STRUCTURE OF PRECIPITATING STRATUS AND PRECIPITATION POTENTIAL IN SPRING IN JILIN PROVINCE. Journal of the Meteorological Sciences,2005,(6):609-616

复制
分享
相关视频

文章指标
  • 点击次数:
  • 下载次数:
  • HTML阅读次数:
  • 引用次数:
历史
  • 收稿日期:2004-11-08
  • 最后修改日期:
  • 录用日期:
  • 在线发布日期:
  • 出版日期:
文章二维码
您是第位访问者
气象科学 ® 2026 版权所有
技术支持:北京勤云科技发展有限公司