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Circuitous attachment process in altitude-triggered lightning striking a 30- 1 m-high tower

机译:高度触发闪电中的迂回连接过程触起了30-1米高的塔架

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摘要

The altitude rocket-and-wire technique was used to trigger lightning to strike a 30-m-high communication tower. A comprehensive dataset was obtained, including discharge current and electromagnetic-field changes, as well as high-speed video images. An attachment process with an abnormal circuitous S-shaped connection channel was observed between the lower extremity of the triggering wire and the tower top, with a total channel length of 25.3 m, which was much longer than the direct connection channel of 13.0 m. The downward negative leader from the triggering wire and the upward connecting positive leader from the tower top "missed" each other by a vertical distance of 4.1 m before turning to the horizontal direction and eventually completing the breakthrough phase. The attachment process produced a sharp current pulse with a duration of 19 is and a peak of 11.6 kA, transiently promoting the upward positive leader development from the upper extremity of the triggering wire. The simulation of the background electric field indicated that the electric field surrounding the tips of the initial leaders did not involve a dominant direction with pronounced larger intensity. The leader streamer/corona zones with a divergent feature resulted in directional uncertainty for the initial steps. As the leaders developed and the associated streamer/corona zones expanded, the attraction effect was enhanced and the leaders turned to the horizontal direction. The common streamer zone (CSZ) developed when the gap between the leaders was about 8 to 9 m, resulting in the occurrence of the breakthrough phase and accomplishment of the attachment. For the last return stroke, the long interstroke interval facilitated channel cooling and a decrease in conductivity. This promoted the occurrence of a dart-stepped leader instead of dart leader, and led to the alteration of the attachment route from an S-shaped channel to a direct connection channel.
机译:高度火箭和线材技术用于触发闪电击打30米高的通信塔。获得了全面的数据集,包括放电电流和电磁场变化,以及高速视频图像。在触发线和塔顶的下端之间观察到具有异常电路S形连接通道的连接过程,总通道长度为25.3米,比13.0米的直接连接通道长得多得多。从触发线的向下负极的引导和从塔顶的向上连接的正极领导,在转向水平方向之前,通过4.1μm的垂直距离,并最终完成突破阶段。附接过程产生持续19的尖锐电流脉冲是11.6ka的峰值,瞬时促进触发线的上末端向上施加的正面展开。背景电场的仿真表明,围绕初始领导者的尖端的电场并不涉及具有明显更大的强度的主导方向。具有发散特征的领导者流/电晕区域导致初始步骤的方向不确定性。随着领导者的开发和相关的拖斯/电晕区扩展,增强了吸引效果,并且领导者转向水平方向。当领导者之间的间隙约为8至9μm时,开发的公共拖缆区(CSZ)产生的突破阶段的发生和附着的成就。对于最后的回流冲程,长的主机间隔便于通道冷却和导电性的降低。这促进了飞镖阶梯式领导者而不是DART领导者的发生,并导致从S形通道到直接连接通道的附接路径的改变。

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  • 来源
    《Atmospheric research 》 |2020年第11期| 105049.1-105049.11| 共11页
  • 作者单位

    Nanjing Univ Informat Sci & Technol Key Lab Aerosol Cloud Precipitat China Meteorol A Collaborat Innovat Ctr Forecast & Evaluat Meteoro Joint Int Res Lab Climate & Environm Change ILCEC Nanjing 210044 Peoples R China;

    Nanjing Univ Informat Sci & Technol Key Lab Aerosol Cloud Precipitat China Meteorol A Collaborat Innovat Ctr Forecast & Evaluat Meteoro Joint Int Res Lab Climate & Environm Change ILCEC Nanjing 210044 Peoples R China|Chinese Acad Sci Inst Atmospher Phys Key Lab Middle Atmosphere & Global Environm Obser Beijing 100029 Peoples R China;

    Chengdu Univ Informat Technol Coll Elect Engn Chengdu 610225 Peoples R China;

    Nanjing Univ Informat Sci & Technol Key Lab Aerosol Cloud Precipitat China Meteorol A Collaborat Innovat Ctr Forecast & Evaluat Meteoro Joint Int Res Lab Climate & Environm Change ILCEC Nanjing 210044 Peoples R China|Chinese Acad Sci Inst Atmospher Phys Key Lab Middle Atmosphere & Global Environm Obser Beijing 100029 Peoples R China|Univ Chinese Acad Sci Coll Earth & Planetary Sci Beijing 100049 Peoples R China;

    Nanjing Univ Informat Sci & Technol Key Lab Aerosol Cloud Precipitat China Meteorol A Collaborat Innovat Ctr Forecast & Evaluat Meteoro Joint Int Res Lab Climate & Environm Change ILCEC Nanjing 210044 Peoples R China;

    Nanjing Univ Informat Sci & Technol Key Lab Aerosol Cloud Precipitat China Meteorol A Collaborat Innovat Ctr Forecast & Evaluat Meteoro Joint Int Res Lab Climate & Environm Change ILCEC Nanjing 210044 Peoples R China;

    Chinese Acad Sci Inst Atmospher Phys Key Lab Middle Atmosphere & Global Environm Obser Beijing 100029 Peoples R China|Univ Chinese Acad Sci Coll Earth & Planetary Sci Beijing 100049 Peoples R China;

    Chinese Acad Sci Inst Atmospher Phys Key Lab Middle Atmosphere & Global Environm Obser Beijing 100029 Peoples R China;

    Chinese Acad Sci Inst Atmospher Phys Key Lab Middle Atmosphere & Global Environm Obser Beijing 100029 Peoples R China;

    Chinese Acad Sci Inst Atmospher Phys Key Lab Middle Atmosphere & Global Environm Obser Beijing 100029 Peoples R China;

    Nanjing Univ Informat Sci & Technol Key Lab Aerosol Cloud Precipitat China Meteorol A Collaborat Innovat Ctr Forecast & Evaluat Meteoro Joint Int Res Lab Climate & Environm Change ILCEC Nanjing 210044 Peoples R China;

    Nanjing Univ Informat Sci & Technol Key Lab Aerosol Cloud Precipitat China Meteorol A Collaborat Innovat Ctr Forecast & Evaluat Meteoro Joint Int Res Lab Climate & Environm Change ILCEC Nanjing 210044 Peoples R China;

    Chinese Acad Sci Inst Atmospher Phys Key Lab Middle Atmosphere & Global Environm Obser Beijing 100029 Peoples R China|Univ Chinese Acad Sci Coll Earth & Planetary Sci Beijing 100049 Peoples R China;

    Civil Aviat Telecommun Dev Co Ltd Beijing 100122 Peoples R China;

    ZTE Corp Shenzhen 518057 Peoples R China;

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