Low Frequency Oscillation Observed in the Ionosphere Around the Substorm Onsets

Abstract Three substorm events in which Defense Meteorological Satellite Program (DMSP) spacecraft are geomagnetically co‐located with substorm onset locations in IMAGE far ultraviolet auroral images are analyzed. A Hilbert‐Huang Transform is used to decompose the DMSP in the ionosphere to its intrinsic mode functions. A dominant mode near 10 mHz shows that its wave instantaneous energy starts increasing 2–5 min prior to and peaks about the commencement of sudden broadband and monoenergetic electron accelerations and the substorm expansion phase. The auroral beads exhibit azimuthal structuring with , which corresponds to the Doppler shifted kinetic ballooning frequency of 3–20 mHz and which is consistent with the 10 mHz wave. The kinetic ballooning mode can become unstable during the substorm growth phase when the pressure gradient and magnetic field‐line curvature become large. The 10 mHz oscillations thus can provide a signature marking approximately the start of the substorm expansion phase.

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Publication Details

Journal
Geophysical Research Letters
Published
2026-01-13
DOI
https://doi.org/10.1029/2025gl115212
Primary Topic
Ionosphere and magnetosphere dynamics
Type
article
Field-Weighted Citation Impact
0.00

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article

Low Frequency Oscillation Observed in the Ionosphere Around the Substorm Onsets

A. J. Hull, P. A. Damiano, S. Wing, Elmer C. Rivera et al.
Geophysical Research Letters
Ionosphere and magnetosphere dynamics
article

Low Frequency Oscillation Observed in the Ionosphere Around the Substorm Onsets

A. J. Hull, P. A. Damiano, S. Wing, Elmer C. Rivera, Jay R. Johnson
article en

Abstract

Abstract Three substorm events in which Defense Meteorological Satellite Program (DMSP) spacecraft are geomagnetically co‐located with substorm onset locations in IMAGE far ultraviolet auroral images are analyzed. A Hilbert‐Huang Transform is used to decompose the DMSP in the ionosphere to its intrinsic mode functions. A dominant mode near 10 mHz shows that its wave instantaneous energy starts increasing 2–5 min prior to and peaks about the commencement of sudden broadband and monoenergetic electron accelerations and the substorm expansion phase. The auroral beads exhibit azimuthal structuring with , which corresponds to the Doppler shifted kinetic ballooning frequency of 3–20 mHz and which is consistent with the 10 mHz wave. The kinetic ballooning mode can become unstable during the substorm growth phase when the pressure gradient and magnetic field‐line curvature become large. The 10 mHz oscillations thus can provide a signature marking approximately the start of the substorm expansion phase.

Geophysical Research LettersVol. 53(2)
Andrews University (US), University of Alaska Fairbanks (US), Johns Hopkins University Applied Physics Laboratory (US), University of California, Berkeley (US)
National Science Foundation, National Aeronautics and Space Administration, Nuclear Safety and Security Commission
Affordable and clean energy
Openalex Percentile: Top 85%
Ionosphere and magnetosphere dynamics
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Low Frequency Oscillation Observed in the Ionosphere Around the Substorm Onsets — A. J. Hull, P. A. Damiano, et al. · Geophysical Research Letters (2026) | TGRS Research Map | TGRS