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Two Propagation Scenarios of Isolated Breakdown Lightning Processes in Failed Negative Cloud‐to‐Ground Flashes
Author(s) -
Kolmašová Ivana,
Santolík Ondřej,
Defer Eric,
Kašpar Petr,
Kolínská Andrea,
Pedeboy Stéphane,
Coquillat Sylvain
Publication year - 2020
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/2020gl090593
Subject(s) - lightning (connector) , waveform , pulse (music) , cloud computing , physics , environmental science , meteorology , optics , voltage , computer science , operating system , power (physics) , quantum mechanics , detector
Isolated breakdown process (also known as attempted leader or inverted intra‐cloud discharge) is a lightning phenomenon characterized by radio wave pulses similar to signatures of preliminary breakdown before negative cloud‐to‐ground flashes, but in this case no cloud‐to‐ground return strokes occur. We identified 128 isolated breakdown pulse trains in measurements collected in the Mediterranean by a broadband receiver (0.005–37 MHz) in 2015 and 2018. By combining these records with concurrent Lightning Mapping Array measurements of very high frequency radiation (60–66 MHz) emitted by in‐cloud discharges we investigate the development of each discharge. We identify two scenarios: Either the discharges continue to propagate almost horizontally for more than 150 ms (73%), or they quickly fade out (27%). The geo‐localized sources of the observed isolated breakdown pulse trains, together with their waveform characteristics (duration, inter‐pulse intervals, regularity, and bipolar shapes) show that both scenarios are similar to initiation processes preceding negative cloud‐to‐ground flashes.