Szczegóły publikacji
Opis bibliograficzny
Observations of elves and radio wave perturbations by intense lightning / Maja Tomicic, Olivier Chanrion, Thomas Farges, Janusz MŁYNARCZYK, Ivana Kolmašová, Serge Soula, Jeff Lapierre, Christoph Köhn, Torsten Neubert // Journal of Geophysical Research [Dokument elektroniczny]. — Czasopismo elektroniczne ; ISSN 2169-8996. Atmospheres ; ISSN 2169-897X. — 2023 — vol. 128 iss. 10 art. no. e2022JD036541, s. 1–20. — Bibliogr. s. 18–20, Abstr. — Publikacja dostępna online od: 2023-05-11
Autorzy (9)
- Tomicic Maja
- Chanrion Olivier
- Farges Thomas
- AGHMłynarczyk Janusz
- Kolmašová Ivana
- Soula Serge
- Lapierre Jeff
- Köhn Christoph
- Neubert Torsten
Dane bibliometryczne
| ID BaDAP | 150275 |
|---|---|
| Data dodania do BaDAP | 2024-01-08 |
| Tekst źródłowy | URL |
| DOI | 10.1029/2022JD036541 |
| Rok publikacji | 2023 |
| Typ publikacji | artykuł w czasopiśmie |
| Otwarty dostęp |  |
| Creative Commons | |
| Czasopismo/seria | Journal of Geophysical Research, Atmospheres |
Abstract
Electromagnetic pulses (EMPs) and quasi-static electric fields (QE) from powerful lightning heat and ionize the lower ionosphere. The EMP disturbance may appear as an elve at ∼80–95 km altitude, and the QE field as a halo or a sprite at ∼60–80 km altitude. Both are thought to perturb crossing radio signals because of changes to the electrical conductivity of the regions. Here we present an analysis of 63 elves and corresponding radio signal perturbations from an almost stationary thunderstorm system that allows us to untangle some of the dependencies of perturbations on the lightning characteristics. The amplitude perturbations of a VLF-transmitter signal are characterized as either long-recovery, early events (LOREs) or as early events. We find that LOREs are related to lightning with high peak currents and bright elves, and that their sign (amplitude increase or decrease) depends on the relative locations of the transmitter, disturbance and receiver. Based on a subset of strokes, lightning with elves has on average ∼3 times the impulse charge-moment-change and power in broadband as lightning of similar peak currents without elves. The early events occur without observed elves, sprites or halos. They recover in ∼10–100 s and are observed for both polarities of cloud-to-ground lightning and for intracloud flashes. It is proposed that these observations may relate to regions of reduced conductivity caused by an electron attachment/detachment process at lower heights, or by electron enhancements associated with TLEs that are too dim to be detected by the camera.
