Processes in negative and positive CG lightning flashes detected from space by GLM
Processes in negative and positive CG lightning flashes detected from space by GLM
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DOI:
10.1016/j.epsr.2024.110183
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发表时间:
2024-04
影响因子:
3.9
通讯作者:
A. Leal;V. Rakov
中科院分区:
文献类型:
--
作者:
A. Leal;V. Rakov
Negative and positive lightning flashes involve a number of different processes, including the preliminary breakdown, stepped and dart leaders, return strokes, continuing currents, M-components, etc. The Geostationary Lightning Mapper (GLM) onboard of Geostationary Operational Environmental Satellites (GOES 16, 17 and 18) is an optical lightning detector with a time resolution of 2 ms and spatial resolution of about 8 km at nadir. The GLM provides three types of data: events, groups, and flashes. According to GLM designers, the group data are intended to track individual lightning strokes. We recorded wideband lightning electric fields using fast and slow antennas in the Amazon and compared them with the corresponding GLM group data (optical energy in Joules) to investigate what lightning processes can be detected from space by GLM. Based on a sample of 15 -CG flashes containing 56 strokes and 15 +CG flashes containing 24 strokes, we found that GLM detected some luminosity in 89 % of 2 ms time windows corresponding to -CG return strokes and 96 % of windows corresponding to +CG return strokes. It also detected luminosity in 100 % of time windows corresponding to preliminary breakdown processes in positive flashes versus 53 % in negative flashes. Further, the GLM detected luminosity emissions associated with 80 % and 40 % of first-stroke leaders in positive and negative flashes, respectively. In general, GLM is more efficient in detecting processes in positive lightning flashes than in negative ones.