2022年春季湖北一次強對流天氣過程雷達衛星閃電觀測特征分析
作者:
作者單位:

作者簡介:

通訊作者:

中圖分類號:

基金項目:

災害天氣國家重點實驗室開放課題(2021LASWB03)和湖北省氣象局面上項目(2021Y01)共同資助


Analysis on Radar Satellite and Lightning Characteristics of a Severe Convective Process in Hubei in the Spring of 2022
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:

    利用衛星、雷達、閃電和NCEP再分析資料等,以湖北省2022年3月16日一次大范圍強對流過程為研究個例,對西南渦移動過程中兩個不同位置對流系統的觀測特征進行了分析。結果表明:槽前西南渦東移是本次強對流的主要影響系統,東部的風雹天氣主要出現在低渦及暖式切變線頂部,南部對流則是由低渦南部冷式切變線誘發。本個例中對流發展初期云頂亮溫TBB逐漸下降到220 K以下,未來1 h TBB變率局部最大可達-30 ℃,大部分閃電緊貼著TBB≤220 K積云右側和TBB變率大值區中心及邊緣,對流系統右側的閃電對于對流系統的發展移動有較好的指示意義;成熟期TBB≤210 K的積云面積達到最大,未來1 h TBB變率減小,密集閃電分布在積云云團中部且隨著TBB低值區移動。雷達觀測反射率因子垂直剖面呈右傾結構,對流發展階段的右傾特征更為明顯,閃電位于對流系統右前側,和≥45 dBz的強回波基本吻合;≥45 dBz、≥50 dBz組合反射率面積,≥10 km、≥12 km回波頂高面積與對流發展演變呈正相關,正、負地閃峰值出現較風雹有0~18 min的時間提前量,負地閃的首次峰值對風雹的提前量可達18 min。

    Abstract:

    Using satellite data, radar data, lightning data and NCEP reanalysis data, taking a large-scale strong convective process in Hubei Province on March 16, 2022 as an example, the observation characteristics of convective systems at two different positions during the movement of the southwest vortex ars analyzed. The results show that the eastward movement of the southwest vortex in front of the trough was the main influence system of the strong convection. The wind and hail weather in eastern Hubei mainly occurred at the top of the low vortex and the warm shear line, while the cold shear line in the southern part of the low vortex induced the southern convection. In this case, the TBB gradually dropped below 220 K in the early stage of convective development, and the maximum local TBB variability could reach -30 ℃ in the next one. Most of the lightning strikes were close to the right side of the TBB≤220 K cumulus and the centre and edge of the large TBB variability area. The lightning on the right side of the convective system was a good indicator of the development and movement of the convective system. The area of cumulus clouds with TBB≤210 K reached the maximum in the mature stage, and the TBB variability decreased in the next hour. The dense lightning strikes were distributed in the middle of the cumulus cloud cluster and moved with the low TBB area. The vertical profile of the radar reflectivity factor presented a right-tilt structure, and the righttilt feature was more evident in the convective development stage. The lightning was located on the right front side of the convective system and was consistent with the strong echo of ≥45 dBz; the combined reflectivity area of ≥45 dBz and ≥50 dBz, and the echo top areas of ≥10 km and≥12 km were positively correlated with the evolution of convective systems. The positive and negative ground lightning peaks appeared 0 to 18 minutes earlier than wind and hail. The first peak value of negative ground lightning significantly impacted wind and hail, and the advance amount could reach 18 minutes.

    參考文獻
    相似文獻
    引證文獻
引用本文

朱傳林,姚雯,茍阿寧,龐文靜,張文剛,李俊.2022年春季湖北一次強對流天氣過程雷達衛星閃電觀測特征分析[J].氣象科技,2023,51(3):431~440

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:2022-06-16
  • 定稿日期:2023-02-07
  • 錄用日期:
  • 在線發布日期: 2023-06-29
  • 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
>