2019
DOI: 10.1038/s41467-019-09621-z
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Fast negative breakdown in thunderstorms

Abstract: Thunderstorms are natural laboratories for studying electrical discharges in air, where the vast temporal, spatial, and energy scales available can spawn surprising phenomena that reveal deficiencies in our understanding of dielectric breakdown. Recent discoveries, such as sprites, jets, terrestrial gamma ray flashes, and fast positive breakdown, highlight the diversity of complex phenomena that thunderstorms can produce, and point to the possibility for electrical breakdown/discharge mechanisms beyond dielect… Show more

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Cited by 85 publications
(183 citation statements)
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References 52 publications
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“…Requiring a reasonable width for the fast breakdown region and an ambient field not too far above ERA thus points to a “zone of plausibility”, as shown in the right panel of Figure , with ambient field near ERA and a fast breakdown region width of roughly 100–300 meters for these two NBEs of approximately 500 meters length. Interferometric measurements of fast breakdown reported by Rison et al () and Tilles et al () seem to suggest a narrow fast breakdown region with an aspect ratio <0.1, which according to this analysis would imply extremely high ambient electric fields. However, by estimating single‐point source locations over time windows of several microseconds that average many thousands (at least) of individual streamers, these measurements only provide the centroid of the VHF emission region.…”
Section: Discussionsupporting
confidence: 81%
“…Requiring a reasonable width for the fast breakdown region and an ambient field not too far above ERA thus points to a “zone of plausibility”, as shown in the right panel of Figure , with ambient field near ERA and a fast breakdown region width of roughly 100–300 meters for these two NBEs of approximately 500 meters length. Interferometric measurements of fast breakdown reported by Rison et al () and Tilles et al () seem to suggest a narrow fast breakdown region with an aspect ratio <0.1, which according to this analysis would imply extremely high ambient electric fields. However, by estimating single‐point source locations over time windows of several microseconds that average many thousands (at least) of individual streamers, these measurements only provide the centroid of the VHF emission region.…”
Section: Discussionsupporting
confidence: 81%
“…The chosen speed, 3×10 7 m/s, is consistent with reported velocities of fast positive (Rison et al, ) and negative (Tilles et al, ) breakdown in thunderstorms. Rison et al () registered speeds typically in the range of 3–23×10 7 m/s for positive‐polarity events observed in a New Mexico storm, roughly 9–10 km above mean sea level.…”
Section: Model Formulationsupporting
confidence: 86%
“…In this work, for the sake of simplicity, we assume that the streamer system propagates at a constant velocity. This is a reasonable assumption according to the observations, which show a roughly linear relationship between height and time during the first 5–15 μs of propagation, when the sources are more intense and the vertical motion can be determined with great accuracy (see, e.g., Rison et al, , Figures 1–2; Tilles et al, , Figures 2–4). In reality, it is expected that the streamer system velocity depends on the electric field at the moving front E , in a similar manner that individual streamers do, but the functional form of v ( E ) is not known.…”
Section: Model Formulationmentioning
confidence: 68%
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