Energy Transport and Conversion Above a Bright Discrete Auroral Arc

Magnetically connected observations of particle distributions and luminosity from the Reimei spacecraft are used to examine energy transport and conversion occurring above a discrete auroral arc. By combining imaging and in situ measurements it is shown how transverse electromagnetic and kinetic energy fluxes measured along the spacecraft trajectory converge across geomagnetic field-lines into the acceleration region. It is shown how cross-field energy transport is facilitated by the formation of vortices along the length of the arc. From an integration over the vertical extent of the acceleration region it is shown that the transverse and field-aligned flow of energy into the arc locally supports the dissipation needed to power the electron acceleration observed. Estimates of gradients in electromagnetic and kinetic energy flows show how field-aligned electron energization in the acceleration region is supported by the divergence of Poynting flux along and across the background magnetic field.

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Publication Details

Journal
Journal of Geophysical Research Space Physics
Published
2024-11-27
DOI
https://doi.org/10.1029/2024ja032870
Citations
1
Primary Topic
Ionosphere and magnetosphere dynamics
Type
article
Field-Weighted Citation Impact
0.33

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article

Energy Transport and Conversion Above a Bright Discrete Auroral Arc

C. C. Chaston
1 citations
Journal of Geophysical Research Space Physics
Ionosphere and magnetosphere dynamics
0.33
article

Energy Transport and Conversion Above a Bright Discrete Auroral Arc

C. C. Chaston
article en
1 citations

Abstract

Magnetically connected observations of particle distributions and luminosity from the Reimei spacecraft are used to examine energy transport and conversion occurring above a discrete auroral arc. By combining imaging and in situ measurements it is shown how transverse electromagnetic and kinetic energy fluxes measured along the spacecraft trajectory converge across geomagnetic field-lines into the acceleration region. It is shown how cross-field energy transport is facilitated by the formation of vortices along the length of the arc. From an integration over the vertical extent of the acceleration region it is shown that the transverse and field-aligned flow of energy into the arc locally supports the dissipation needed to power the electron acceleration observed. Estimates of gradients in electromagnetic and kinetic energy flows show how field-aligned electron energization in the acceleration region is supported by the divergence of Poynting flux along and across the background magnetic field.

Journal of Geophysical Research Space PhysicsVol. 129(12)
University of California, Berkeley (US)
U.S. Department of Energy
Affordable and clean energy
Openalex Percentile: Top 33%
Ionosphere and magnetosphere dynamics
0.33
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