Szczegóły publikacji

Opis bibliograficzny

Quantification of perturbation to the daytime lower ionosphere from a gamma ray burst using ELF remote sensing / M. Gołkowski, Z. Nieckarz, J. MŁYNARCZYK, M. Ostrowski, J. Kubisz, A. Michalec, J. Lichtenberger, A. Klekociuk, P. Nicholson // Geophysical Research Letters ; ISSN  0094-8276 . — 2025 — vol. 52 iss. 22 art. no. e2025GL117989, s. 1–8. — Bibliogr. s. 7–8, Abstr. — Publikacja dostępna online od: 2025-11-11

Autorzy (9)

  • Gołkowski Marek
  • Nieckarz Zenon
  • AGHMłynarczyk Janusz
  • Ostrowski Michał
  • Kubisz Jerzy
  • Michalec Adam
  • Lichtenberger J.
  • Klekociuk A.
  • Nicholson P.

Słowa kluczowe

D region ionosphereremote sensingSchumann resonanceslightninggamma ray burstELF impulses

Dane bibliometryczne

ID BaDAP164759
Data dodania do BaDAP2025-12-15
Tekst źródłowyURL
DOI10.1029/2025GL117989
Rok publikacji2025
Typ publikacjiartykuł w czasopiśmie
Otwarty dostęptak
Creative Commons
Czasopismo/seriaGeophysical Research Letters

Abstract

On 9 October 2022, a powerful gamma ray burst (GRB), GRB221009A, caused significant changes in the electron density of the lower ionosphere, as evidenced by VLF (3–30 kHz) radio wave observations. However, GRB221009A did not yield any observable signatures at the Schumann resonances (∼8, ∼14 Hz), which are also sensitive to the lower ionosphere. We show that the effects of GRB221009A are observable in a decrease in propagation velocity of ELF (3–1,000 Hz) lightning impulses. Analytical and numerical analysis points to an ionospheric perturbation in which the GRB increased the daytime electron density uniformly over a wide altitude range from 50 to 90 km. The GRB perturbation is markedly different from perturbations from solar flares, which significantly increase the vertical gradient of the electron density. ELF propagation velocity is shown to be a technique that can identify the altitude range of ionospheric perturbations.