Effects of a Solar Flare on Global Propagation of Extremely Low Frequency Waves

Abstract Solar flares have profound impacts on the lower ionosphere and long‐distance radio propagation. Extremely low frequency (ELF: 3–3,000 Hz) waves are challenging to observe and experience unique interactions with the lower ionosphere. The primary natural sources of ELF waves are thunderstorm lightnings across the globe. Using a newly developed azimuth determination technique and improved observation hardware we show that ELF attenuation in the Earth‐Ionosphere spherical cavity decreases and propagation velocity increases under the influence of an M‐class solar flare. Using a two‐parameter model of the lower ionosphere, the observations are shown to be consistent with increased electron density and sharper gradients in the D‐region resulting from X‐ray radiation. The sharper electron density gradient is primarily responsible for the propagation velocity increase, suggesting a unique capability that ELF observations can bring to global remote sensing of the lower ionosphere under space weather perturbations.

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Publication Details

Journal
Journal of Geophysical Research Space Physics
Published
2024-12-01
DOI
https://doi.org/10.1029/2024ja033083
Citations
3
Primary Topic
Ionosphere and magnetosphere dynamics
Type
article
Field-Weighted Citation Impact
0.99
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article

Effects of a Solar Flare on Global Propagation of Extremely Low Frequency Waves

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3 citations
Journal of Geophysical Research Space Physics
Ionosphere and magnetosphere dynamics
0.99
article

Effects of a Solar Flare on Global Propagation of Extremely Low Frequency Waves

János Lichtenberger, Zenon Nieckarz, Mark Gołkowski, Ashanthi Maxworth, M. Ostrowski, A. Michalec, Janusz Młynarczyk, Jerzy Kubisz
article en
3 citations

Abstract

Abstract Solar flares have profound impacts on the lower ionosphere and long‐distance radio propagation. Extremely low frequency (ELF: 3–3,000 Hz) waves are challenging to observe and experience unique interactions with the lower ionosphere. The primary natural sources of ELF waves are thunderstorm lightnings across the globe. Using a newly developed azimuth determination technique and improved observation hardware we show that ELF attenuation in the Earth‐Ionosphere spherical cavity decreases and propagation velocity increases under the influence of an M‐class solar flare. Using a two‐parameter model of the lower ionosphere, the observations are shown to be consistent with increased electron density and sharper gradients in the D‐region resulting from X‐ray radiation. The sharper electron density gradient is primarily responsible for the propagation velocity increase, suggesting a unique capability that ELF observations can bring to global remote sensing of the lower ionosphere under space weather perturbations.

Journal of Geophysical Research Space PhysicsVol. 129(12)
Eötvös Loránd University (HU), Jagiellonian University (PL), Institute of Physics (PL), AGH University of Krakow (PL), University of Southern Maine (US), University of Colorado Denver (US)
Openalex Percentile: Top 22%
Ionosphere and magnetosphere dynamics
0.99
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