都江堰短時強降水時空分布統計分析
DOI:
作者:
作者單位:

作者簡介:

通訊作者:

中圖分類號:

基金項目:

“滑坡泥石流”行業專項(“GYHY201006040”)資助


Temporal Spatial Distribution Characteristics of Short Period Heavy Precipitation in Dujiangyan
Author:
Affiliation:

Fund Project:

  • 摘要
  • |
  • 圖/表
  • |
  • 訪問統計
  • |
  • 參考文獻
  • |
  • 相似文獻
  • |
  • 引證文獻
  • |
  • 資源附件
  • |
  • 文章評論
    摘要:

    根據氣象觀測站逐5 min雨量資料的統計結果,分析了四川都江堰地區短時強降水的時空分布變化特征,結果表明:①都江堰各年1 h雨量極值均出現在較高海拔的地區,且1 h雨量極值在當次降水過程總雨量中所占的比重很高,說明都江堰短時強降水的強度非常集中;②受地形與夜間云頂輻射冷卻作用,都江堰短時強降水的夜雨特征突出,且后半夜比前半夜多;③都江堰地區夏季的對流過程一般是沿西北山脈迎風坡生成與發展的,隨后對流系統發展到東南平原地區;④都江堰短時強降水主要集中在60~130 min,最長可持續210 min。

    Abstract:

    The statistical results from the rain gauge data extracted every 5 minutes are used to analyze the temporal spatial distribution variations of short period heavy precipitation in Dujiangyan. The results show: (1) the maximum of hourly rainfall occurs usually in high altitude areas. The maximum hourly rainfall has a big weight in total precipitation in the same event, which reflects that the rainfall in Dujiangyan is characterized by high intensity and concentrative precipitation time. (2) Influenced by the effect of landform and the radiative cooling of cloud tops, short period heavy precipitation in Dujiangyan primarily occurs at night, and there occur more freguently rains after midnight than before midnight. (3) Heavy precipitation occurs first along the windward slope of the mountains in summer, and afterwards,convection systems move towards southeast areas. (4) The durations of short period heavy precipitation in Dujiangyan are calculated. The precipitation duration ranges from 60 to 130 minutes generally, with the maximum up to 210 minutes.

    參考文獻
    相似文獻
    引證文獻
引用本文

袁晨,馬力.都江堰短時強降水時空分布統計分析[J].氣象科技,2013,41(6):1086~1090

復制
分享
文章指標
  • 點擊次數:
  • 下載次數:
  • HTML閱讀次數:
  • 引用次數:
歷史
  • 收稿日期:2012-12-24
  • 定稿日期:2013-05-21
  • 錄用日期:
  • 在線發布日期: 2013-12-27
  • 出版日期:
您是第位訪問者
技術支持:北京勤云科技發展有限公司
午夜欧美大片免费观看,欧美激情综合五月色丁香,亚洲日本在线视频观看,午夜精品福利在线
>