Lightning Characteristics and Electric Charge Structure of a Hail-Producing Thunderstorm on the Eastern Qinghai–Tibetan Plateau
An isolated hail-producing thunderstorm that occurred on 20 August 2012, from the Composite Observing Experiment for Lightning project carried out in the Da Tong Region of Qinghai Province, China, was studied. In most stages, the charge structure in the storm showed a positive tripole structure, whi...
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doaj-a2982955b2e74a2ba176146b59fdeec92020-11-24T22:06:50ZengMDPI AGAtmosphere2073-44332018-07-019829510.3390/atmos9080295atmos9080295Lightning Characteristics and Electric Charge Structure of a Hail-Producing Thunderstorm on the Eastern Qinghai–Tibetan PlateauXiangpeng Fan0Yijun Zhang1Guangshu Zhang2Dong Zheng3State Key Laboratory of Severe Weather/Laboratory of Lightning Physics and Protection Engineering, Chinese Academy of Meteorological Sciences, Beijing 100081, ChinaState Key Laboratory of Severe Weather/Laboratory of Lightning Physics and Protection Engineering, Chinese Academy of Meteorological Sciences, Beijing 100081, ChinaKey Laboratory of Land Surface Process and Climate Change in Cold and Arid Regions, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, ChinaState Key Laboratory of Severe Weather/Laboratory of Lightning Physics and Protection Engineering, Chinese Academy of Meteorological Sciences, Beijing 100081, ChinaAn isolated hail-producing thunderstorm that occurred on 20 August 2012, from the Composite Observing Experiment for Lightning project carried out in the Da Tong Region of Qinghai Province, China, was studied. In most stages, the charge structure in the storm showed a positive tripole structure, which resulted in a low positive ground lightning rate for the whole event. In the thunderstorm process, 202 lightning flashes were detected. The peak lightning rate of lightning was 28 times/5 min. The average number of return strokes of negative ground flash was 2.4, and only one return stroke of positive ground lightning occurred. The duration of the in-cloud process prior to the first return stroke was relatively long. Dynamic transport had a considerable influence on the charge structure of the cloud. Before and after hail landing, the ground electric field of several stations showed a consistent trend of reversal.http://www.mdpi.com/2073-4433/9/8/295hail-producing orographic thunderstormlightning mappingvery high frequency (VHF) radiationcharge structuretotal lightning rate |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Xiangpeng Fan Yijun Zhang Guangshu Zhang Dong Zheng |
spellingShingle |
Xiangpeng Fan Yijun Zhang Guangshu Zhang Dong Zheng Lightning Characteristics and Electric Charge Structure of a Hail-Producing Thunderstorm on the Eastern Qinghai–Tibetan Plateau Atmosphere hail-producing orographic thunderstorm lightning mapping very high frequency (VHF) radiation charge structure total lightning rate |
author_facet |
Xiangpeng Fan Yijun Zhang Guangshu Zhang Dong Zheng |
author_sort |
Xiangpeng Fan |
title |
Lightning Characteristics and Electric Charge Structure of a Hail-Producing Thunderstorm on the Eastern Qinghai–Tibetan Plateau |
title_short |
Lightning Characteristics and Electric Charge Structure of a Hail-Producing Thunderstorm on the Eastern Qinghai–Tibetan Plateau |
title_full |
Lightning Characteristics and Electric Charge Structure of a Hail-Producing Thunderstorm on the Eastern Qinghai–Tibetan Plateau |
title_fullStr |
Lightning Characteristics and Electric Charge Structure of a Hail-Producing Thunderstorm on the Eastern Qinghai–Tibetan Plateau |
title_full_unstemmed |
Lightning Characteristics and Electric Charge Structure of a Hail-Producing Thunderstorm on the Eastern Qinghai–Tibetan Plateau |
title_sort |
lightning characteristics and electric charge structure of a hail-producing thunderstorm on the eastern qinghai–tibetan plateau |
publisher |
MDPI AG |
series |
Atmosphere |
issn |
2073-4433 |
publishDate |
2018-07-01 |
description |
An isolated hail-producing thunderstorm that occurred on 20 August 2012, from the Composite Observing Experiment for Lightning project carried out in the Da Tong Region of Qinghai Province, China, was studied. In most stages, the charge structure in the storm showed a positive tripole structure, which resulted in a low positive ground lightning rate for the whole event. In the thunderstorm process, 202 lightning flashes were detected. The peak lightning rate of lightning was 28 times/5 min. The average number of return strokes of negative ground flash was 2.4, and only one return stroke of positive ground lightning occurred. The duration of the in-cloud process prior to the first return stroke was relatively long. Dynamic transport had a considerable influence on the charge structure of the cloud. Before and after hail landing, the ground electric field of several stations showed a consistent trend of reversal. |
topic |
hail-producing orographic thunderstorm lightning mapping very high frequency (VHF) radiation charge structure total lightning rate |
url |
http://www.mdpi.com/2073-4433/9/8/295 |
work_keys_str_mv |
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