Attachment processes of negative flashes with multiple return strokes to a tall tower observed at close distances

IF 4.5 2区 地球科学 Q1 METEOROLOGY & ATMOSPHERIC SCIENCES Atmospheric Research Pub Date : 2024-08-30 DOI:10.1016/j.atmosres.2024.107661
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Abstract

Two downward negative flashes (F1612 & F1613) with multiple return strokes struck to the 356-m Shenzhen Tower were analyzed. The high-speed camera captured upward positive connecting leaders (UCL) for the first strokes of both flashes and two subsequent strokes of F1612. The observations also show that none of the downward negative leader (DNL) completely propagated to the tower tip before the occurrence of the return stroke (RS), so that we inferred that the UCL initiated from the tower tip might exist for each RS of the two flashes. The possible height of the UCL and DNL connecting point above the tower tip for each RS was estimated, which showed a positive correlation to the speed of corresponding DNL. The striking distances estimated for 8 subsequent RSs in F1612 were in a range from 14.6 m to 85.4 m and that for 3 subsequent RSs in F1613 were from 24.2 m to 66.2 m. There was a weak positive linear relationship between the DNL speed and striking distance for subsequent RSs in the two flashes. The DNL speed showed a positive correlation to the peak current of corresponding RS.

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近距离观察高塔上带有多个返回冲程的负闪光的附着过程
分析了打向 356 米高的深圳塔的两次下行负向闪光(F1612 & F1613)的多次回波。高速摄像机捕捉到了这两次闪光的第一个冲程和 F1612 的两个后续冲程的向上正连接前导(UCL)。观测结果还显示,在返回冲程(RS)发生之前,没有一个向下的负前导(DNL)完全传播到塔尖,因此我们推断,在两次闪光的每个 RS 中,都可能存在从塔尖开始的 UCL。我们估算了每个 RS 的 UCL 和 DNL 连接点在塔尖上方的可能高度,结果显示与相应 DNL 的速度呈正相关。F1612 中 8 个后续 RS 的撞击距离估计值介于 14.6 米至 85.4 米之间,F1613 中 3 个后续 RS 的撞击距离估计值介于 24.2 米至 66.2 米之间。DNL 速度与相应 RS 的峰值电流呈正相关。
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来源期刊
Atmospheric Research
Atmospheric Research 地学-气象与大气科学
CiteScore
9.40
自引率
10.90%
发文量
460
审稿时长
47 days
期刊介绍: The journal publishes scientific papers (research papers, review articles, letters and notes) dealing with the part of the atmosphere where meteorological events occur. Attention is given to all processes extending from the earth surface to the tropopause, but special emphasis continues to be devoted to the physics of clouds, mesoscale meteorology and air pollution, i.e. atmospheric aerosols; microphysical processes; cloud dynamics and thermodynamics; numerical simulation, climatology, climate change and weather modification.
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