華南前汛期垂直溫差與強對流天氣發生頻率
DOI:
作者:
作者單位:

作者簡介:

通訊作者:

中圖分類號:

基金項目:

中國氣象局預報員專項項目(CMAYBY2011 037)資助


Vertical Temperature Differences and Ocurrence Frequencies of Strong Convections during Pre Rainy Season
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:

    利用2004—2009年3—6月清遠站探空資料,得到垂直方向11種溫差,對它們與強對流的相關性進行統計,選出相關性較高的850與700、850與500、400與100 hPa等壓面垂直溫度(〖WTBX〗T〖WTBZ〗(850-700)、〖WTBX〗T〖WTBZ〗(850-500)和〖WTBX〗T〖WTBZ〗(400-100))進行研究,對其在各區間出現強對流的頻率進行統計。結果表明,不同月份強對流日低空溫差變化幅度較小,高空溫差變化幅度較大;隨著低空溫差和高空溫差的增加,強對流的頻率基本上呈增加的趨勢;強對流主要集中在〖WTBX〗T〖WTBZ〗(850-500)>20 ℃、〖WTBX〗T〖WTBZ〗(850-700)>6 ℃的區域,〖WTBX〗T〖WTBZ〗(400-100)為64~66 ℃、〖WTBX〗T〖WTBZ〗(850-500)為23~26 ℃、〖WTBX〗T〖WTBZ〗(850-700)為8~11 ℃ 的區域頻率更高;對于大范圍強對流天氣,〖WTBX〗T〖WTBZ〗(850-500)>24 ℃或〖WTBX〗T〖WTBZ〗(850-700)達到10 ℃時,通常是風雨相伴,大范圍強降水為主的可能性極?。弧糤TBX〗T〖WTBZ〗(400-100)<60 ℃時,出現大范圍強降水的可能性非常小。

    Abstract:

    Based on the sounding data of Qingyuan Station from May to October from 2004 to 2009,11 kinds of vertical temperature differences are studied. The correlations between temperature differences and severe convective events are calculated and three kinds with higher correlations are further studied. The occurrence frequencies of severe convective events with different temperature differences are analyzed. The results show that temperature differences in severe convection days at lower altitudes in different months are small, compared with distinct amplitude at high altitudes. The frequencies of severe convective events increased with the increasing of temperature differences at both low and high altitudes. Severe convective events mainly occurred when the temperature difference between 850 hPa and 500 hPa was no less than 20 ℃, and that between 850 hPa and 700 hPa was no less than 6 ℃. When temperature difference between 400 hPa and 100 hPa was between 64 ℃ and 66 ℃ and that between 850 hPa and 500 hPa was between 23 and 26 ℃ or temperature difference between 850 hPa and 700 hPa was between 8 ℃ and 11 ℃, the frequeny would be the highest. As for large scale convective events when temperature difference between 850 hPa and 500 hPa was equal or greater than 24 ℃ or temperature difference between 850 hPa and 700 hPa reached 10 ℃,usually there was gale accompanied with heavy precipitation. When temperature difference between 400 hPa and 100 hPa was less than 60 ℃, the probability of large scale heavy precipitation would be very little.

    參考文獻
    相似文獻
    引證文獻
引用本文

葉愛芬,李懷宇,羅聰,龐古乾,伍志方.華南前汛期垂直溫差與強對流天氣發生頻率[J].氣象科技,2013,41(2):307~313

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:2011-12-20
  • 定稿日期:2012-04-05
  • 錄用日期:
  • 在線發布日期: 2013-04-11
  • 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
>