Articles | Volume 23, issue 12
https://doi.org/10.5194/nhess-23-3747-2023
https://doi.org/10.5194/nhess-23-3747-2023
Research article
 | 
04 Dec 2023
Research article |  | 04 Dec 2023

Characteristics of cloud-to-ground lightning (CG) and differences between +CG and −CG strokes in China regarding the China National Lightning Detection Network

Ruijiao Jiang, Guoping Zhang, Shudong Wang, Bing Xue, Zhengshuai Xie, Tingzhao Yu, Kuoyin Wang, Jin Ding, and Xiaoxiang Zhu

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Cited articles

Carey, L. D. and Buffalo, K. M.: Environmental control of cloud-to-ground lightning polarity in severe storms, Mon. Weather Rev., 135, 1327—1353, 2007. 
Cummins, K. L., Murphy, M. J., Bardo, E. A., Hiscox, W. L., Pyle, R. B., and Pifer, A. E.: A combined TOA/MDF technology upgrade of the US National Lightning Detection Network, J. Geophys. Res.-Atmos., 103, 9035–9044, 1998. 
Diendorfer, G.: Some comments on the achievable accuracy of local ground flash density values, in: International Lightning Detection Conference, June 2008, Uppsala, Sweden, 2008. 
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Short summary
Lightning activity in China is analyzed. Low latitudes, undulating terrain, seaside, and humid surfaces are beneficial for lightning occurrence. Summer of the year or afternoon of the day is the high period. Large cloud-to-ground lightning frequency always corresponds to a small ratio and weak intensity of positive cloud-to-ground lightning on either a temporal or spatial scale. Interestingly, the discharge intensity difference between the two types of lightning shrinks on the Tibetan Plateau.
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