Upgraded Low-Frequency 3D Lightning Mapping System in North China and Observations on Lightning Initiation Processes

Author:

Liu Mingyuan12ORCID,Qie Xiushu12,Sun Zhuling1ORCID,Jiang Rubin1,Zhang Hongbo1,Chen Ruiling12,Yuan Shanfeng1ORCID,Wang Yu34,Liu Xiangke5

Affiliation:

1. Key Laboratory of Middle Atmosphere and Global Environment Observation, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China

2. College of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing 100049, China

3. State Grid Electric Power Research Institute Wuhan NARI Limited Liability Company, Wuhan 430206, China

4. State Grid Electric Power Research Institute Co., Ltd., Nanjing 211199, China

5. Key Laboratory for Meteorological Disaster Prevention and Mitigation of Shandong Province, Jinan 250031, China

Abstract

The three-dimensional (3D) low-frequency lightning mapping system (LF-LMS) in north China has been updated. The lightning electric field derivative (dE/dt) sensor and continuous acquisition mode has been newly designed to ensure a capability of entire lightning processes detection, especially weak discharges during lightning the initiation process. The twice cross-correlation delay estimation and the grid iteration nested optimization location algorithm are used to realize the 3D location of the discharge channel, and the location resolution and calculation speed are balanced consequently. The location results of the rocket-triggered lightning demonstrated that the system achieved a high-resolution mapping of lightning discharge channels, which coincided well with the optical images. The horizontal and vertical location error for rocket triggered lightning was less than 40 m in both horizontal and vertical. Intracloud (IC) lightning flashes were observed to be initiated by three different discharge processes, initial breakdown pulse (IBP), narrow bipolar event (NBE), and initial E-change (IEC). The corresponding initial height was 10.5 km, 6.9 km, and 9.2 km, respectively. The upward negative leader was initially located, followed by scatter radiation sources and negative recoil leaders in the lower negative charge region for all cases. The electric field characteristics of the IEC and subsequent IBPs indicated that they are different discharge processes with the same current direction. The IEC process might correspond to the discharge process with continuous current and less noticeable current changes.

Funder

National Natural Science Foundation of China

Publisher

MDPI AG

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