Abstract

We started a long-term continuous observation of lightning discharges in the Chinese inland plateau region using a fast antenna lightning mapping array (FALMA). During the first year of observation, 2019, we recorded lightning discharges on 25 days in Yinchuan city, the capital of Ningxia. Most of the lightning discharges appeared to occur in the afternoons of individual thunderstorm days in August. We studied the cloud-to-ground (CG) flash percentages, lightning discharge source spatiotemporal distributions, and preliminary breakdown (PB) process characteristics for the two thunderstorm cases that produced the most frequent lightning flashes in 2019 over a wide area. It was found that (1) CG flashes in these two thunderstorms accounted for 28.4% and 32.5% of total lightning flashes, respectively; (2) most lightning discharge sources in these two thunderstorms occurred at temperatures between 5 and −30 °C, with a peak at around −10 °C; and (3) more than 90% of well-mapped PB processes of intracloud (IC) flashes propagated downward. By overlapping the altitudes and the progression directions of the PB processes on the lightning source spatiotemporal distributions, we inferred that the main negative charge of the two storms observed in Ningxia, China, was at a height of around −15 to −25 °C (7 to 9 km) and the main positive charge was at a height of around 5 to 0 °C (2 to 4 km).

Highlights

  • IntroductionIt has been known for over 30 years that the thunderstorms occurring in the Chinese inland plateau region usually produce dominant electric fields on the ground with polarity opposite to that of ordinary summer thunderstorms in low-altitude areas [1,2]

  • By overlapping the altitudes and the progression directions of the preliminary breakdown (PB) processes on the lightning source spatiotemporal distributions, we inferred that the main negative charge of the two storms observed in Ningxia, China, was at a height of around −15 to −25 ◦ C (7 to 9 km) and the main positive charge was at a height of around 5 to 0 ◦ C (2 to 4 km)

  • The main to −25 ◦ C and the main positive charge was at a height of around 5 to charge structures in the two thunderclouds in Ningxia, China, were apparently upside

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Summary

Introduction

It has been known for over 30 years that the thunderstorms occurring in the Chinese inland plateau region usually produce dominant electric fields on the ground with polarity opposite to that of ordinary summer thunderstorms in low-altitude areas [1,2]. It is apparently necessary to install a 3D lightning mapping system which covers a plateau area much wider than that investigated previously [10,11,12], but which is close to lowland areas. In order to find out the optimum protection measures for plateau lightning, the RS characteristics apparently need to be investigated and widely across the plateau area. As shown in [17,18], the fast antenna lightning mapping array system (FALMA) can perform

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