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Peer-reviewedCC BY 4.0Geophysical Research Letters

Weak Positive Discharges Leading to Lightning Initiation

Abstract

Lightning‐initiating events in the Earth's atmosphere originate within compact regions of space with dimensions on the order of hundreds of meters. In the strongest events the associated current pulses propagate from positive to negative thundercloud charge centers at speeds approaching one tenth of the speed of light, a process referred to as fast positive breakdown. Growing observational evidence indicates that these discharges can also develop with much lower current magnitudes and substantially slower propagation speeds. Here we present a quantitative analysis of weak photoelectric feedback discharges (Pasko et al., 2025, https://doi.org/10.1029/2025JD043897 ) that provides an accurate quantitative interpretation of the available observations in terms of current moments, pulse durations, and positive breakdown velocities. Similarly to volt‐ampere characteristics in conventional discharges the photoelectric feedback discharges exhibit a threshold type quadratic dependence on applied electric field explaining observed broad variability of parameters of these discharges.

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BibTeX
@article{pasko2026weak,
  title = {{Weak Positive Discharges Leading to Lightning Initiation}},
  author = {Victor P Pasko and Sebastien Celestin and Anne Bourdon},
  journal = {Geophysical Research Letters},
  year = {2026},
  month = oct,
  doi = {10.1029/2026gl125703},
  url = {https://hal.science/hal-05804173v1},
  note = {CC BY 4.0},
}
RIS
TY  - JOUR
TI  - Weak Positive Discharges Leading to Lightning Initiation
AU  - Victor P Pasko
AU  - Sebastien Celestin
AU  - Anne Bourdon
PY  - 2026
DA  - 2026/10/12
JO  - Geophysical Research Letters
DO  - 10.1029/2026gl125703
UR  - https://hal.science/hal-05804173v1
AB  - Lightning‐initiating events in the Earth's atmosphere originate within compact regions of space with dimensions on the order of hundreds of meters. In the strongest events the associated current pulses propagate from positive to negative thundercloud charge centers at speeds approaching one tenth of the speed of light, a process referred to as fast positive breakdown. Growing observational evidence indicates that these discharges can also develop with much lower current magnitudes and substantially slower propagation speeds. Here we present a quantitative analysis of weak photoelectric feedback discharges (Pasko et al., 2025, https://doi.org/10.1029/2025JD043897 ) that provides an accurate quantitative interpretation of the available observations in terms of current moments, pulse durations, and positive breakdown velocities. Similarly to volt‐ampere characteristics in conventional discharges the photoelectric feedback discharges exhibit a threshold type quadratic dependence on applied electric field explaining observed broad variability of parameters of these discharges.
SN  - 0094-8276
SN  - 1944-8007
ER  -