A Multi‐Platform Statistical Analysis of the Azimuthal Spatial Extent of the Microburst Precipitation Region

Abstract Microbursts are impulsive injections of energetic (few keV to >MeV) electrons into the atmosphere, primarily caused by nonlinear scattering driven by whistler mode chorus waves. While the relative importance of microburst precipitation as a loss process has not been fully quantified, many studies have shown microbursts may play a significant role in the loss of outer radiation belt electrons. We present a multi‐platform statistical analysis of chorus and energetic electron precipitation in an attempt to constrain the azimuthal spatial extent (MLT) of the microburst precipitation region and determine how this extent varies with geomagnetic activity. Statistical upper bounds of this azimuthal extent are determined with observations of general energetic electron precipitation that can include direct microburst detections, while statistical lower bounds determination requires direct microburst detections. The resulting distributions of both upper and lower bounds azimuthal extent suggest that microbursts may frequently constitute an important source of electron loss from the outer radiation belt. We find that 36% of upper bound events in the dawn sector span more than 5 hr in MLT. This azimuthal extent increases with geomagnetic activity, particularly in the dawn and noon MLT sectors.

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Publication Details

Journal
Journal of Geophysical Research Space Physics
Published
2024-12-01
DOI
https://doi.org/10.1029/2024ja033208
Citations
2
Primary Topic
Ionosphere and magnetosphere dynamics
Type
article
Field-Weighted Citation Impact
0.66
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article

A Multi‐Platform Statistical Analysis of the Azimuthal Spatial Extent of the Microburst Precipitation Region

Kelly A. Cantwell, Yoshiya Kasahara, S. S. Elliott, Shoya Matsuda et al.
2 citations
Journal of Geophysical Research Space Physics
Ionosphere and magnetosphere dynamics
0.66
article

A Multi‐Platform Statistical Analysis of the Azimuthal Spatial Extent of the Microburst Precipitation Region

Kelly A. Cantwell, Yoshiya Kasahara, S. S. Elliott, Shoya Matsuda, Iku Shinohara, Alexa Halford, Riley Troyer, C. A. Cattell, A. W. Breneman, Joshua Pettit, R. M. Millan, J. G. Sample, Tomoaki Hori, C. A. Colpitts, Ayako Matsuoka, Mykhaylo Shumko, Yoshizumi Miyoshi, A. Johnson
article en
2 citations

Abstract

Abstract Microbursts are impulsive injections of energetic (few keV to >MeV) electrons into the atmosphere, primarily caused by nonlinear scattering driven by whistler mode chorus waves. While the relative importance of microburst precipitation as a loss process has not been fully quantified, many studies have shown microbursts may play a significant role in the loss of outer radiation belt electrons. We present a multi‐platform statistical analysis of chorus and energetic electron precipitation in an attempt to constrain the azimuthal spatial extent (MLT) of the microburst precipitation region and determine how this extent varies with geomagnetic activity. Statistical upper bounds of this azimuthal extent are determined with observations of general energetic electron precipitation that can include direct microburst detections, while statistical lower bounds determination requires direct microburst detections. The resulting distributions of both upper and lower bounds azimuthal extent suggest that microbursts may frequently constitute an important source of electron loss from the outer radiation belt. We find that 36% of upper bound events in the dawn sector span more than 5 hr in MLT. This azimuthal extent increases with geomagnetic activity, particularly in the dawn and noon MLT sectors.

Journal of Geophysical Research Space PhysicsVol. 129(12)
Kanazawa University (JP), Dartmouth College (US), University of Minnesota (US), Goddard Space Flight Center (US), Montana State University (US), Johns Hopkins University Applied Physics Laboratory (US), National Sagamihara Hospital (JP), Utah State University Space Dynamics Laboratory, Nagoya University (JP)
Openalex Percentile: Top 27%
Ionosphere and magnetosphere dynamics
0.66
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