Abstract

The initiation of a leader is an important lightning discharge process, but how an upward positive leader (UPL) initiates is still not fully understood. The evolution characteristics of a UPL during its initial stage was systematically studied based on directly measured current data of 14 triggered lightning events in 2019. It was found that the initial stage of triggered lightning can be divided into two types: a single initial process form and a multiple initial process form, with percentages of 64.29% and 35.71%, respectively. Compared with the former, the latter usually lasts longer, and the corresponding lightning is often triggered under a lower ground-level quasi-static electric field. In each initial process, precursor current pulses (PCPs), PCP clusters and initial precursor current pulse (IPCPs) are typical current waveforms, and the pulse durations and transferred charges of PCPs increase linearly with time. However, in the multiple initial process form, the pulse durations and transferred charges of PCPs will reduce significantly after each previous initial process and then continue to increase in the following initial process. In each initial process, when the pulse duration and transferred charge of a PCP increase to a certain extent, PCP clusters and IPCPs begin to appear. For the emergence of PCP clusters, the average values of the threshold are 3.48 μs and 19.53 μC, respectively. For the occurrence of IPCPs, the corresponding values are 4.69 μs and 27.23 μC, respectively. The average values of pulse durations and transferred charges of IPCPs are larger than those of PCP clusters. Compared with adjacent PCP clusters, IPCPs contain more pulses, with a critical range of 6–7. IPCPs also last longer, and have a critical range of 138–198 μs.

Highlights

  • In recent years, how an upward positive leader (UPL) initiates has become an important problem in lightning physics research

  • We study the evolution characteristics of UPLs during the initial stage based on directly measured current data of triggered lightning in 2019

  • One of them took the form of a single precursor current pulses (PCPs)–initial precursor current pulses (IPCPs) in the current signal during the initial stage; that is, there was only one IPCPs process

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Summary

Introduction

How an upward positive leader (UPL) initiates has become an important problem in lightning physics research. Due to the randomness of natural lightning, it is difficult to make close observations. The discharge process of triggered lightning is very similar to that of natural lightning, and the timing and location of triggered lightning can be planned, making it easy to observe at close range. In the field of high voltage technology, a long air gap discharge can be used to simulate lightning [1,2,3,4,5,6]. Some conversion threshold parameters during the evolution process of leader are given, such as local electric field, charge per unit length and critical length, but the scale of a long air Atmosphere 2020, 11, 658; doi:10.3390/atmos11060658 www.mdpi.com/journal/atmosphere

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