Unexpected STEVE Observations at High Latitude During Quiet Geomagnetic Conditions

Abstract Strong Thermal Emission Velocity Enhancement (STEVE), is a captivating optical phenomenon typically observed in the mid‐latitude ionosphere. This paper presents an intriguing observation of a STEVE event at high‐latitudes, approximately 10 degrees poleward of previously documented observations. This event was recorded in Yellowknife, Canada, by a TREx RGB imager and a citizen scientist. Swarm satellites traversed the latitude of the observation, measuring extreme westwards ion drift velocities exceeding 4 km/s. Such velocities are more typically associated with the subauroral region located at mid‐latitudes, rather than at the high‐latitudes reported here. Significantly, this event occurred without a substorm, which differs from previous STEVE observations. While high‐latitude radars detected fast ionospheric equatorward flows, GOES satellite did not record any injections. These observations suggest that the inner magnetosphere is highly inflated. This unique case study raises new questions surrounding subauroral dynamics and the influence of magnetospheric configurations on ionospheric responses.

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Publication Details

Journal
Geophysical Research Letters
Published
2024-10-08
DOI
https://doi.org/10.1029/2024gl110568
Citations
6
Primary Topic
Ionosphere and magnetosphere dynamics
Type
article
Field-Weighted Citation Impact
1.99

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article

Unexpected STEVE Observations at High Latitude During Quiet Geomagnetic Conditions

E. Donovan, V. A. Pinto, J. K. Burchill, D. J. Knudsen et al.
6 citations
Geophysical Research Letters
Ionosphere and magnetosphere dynamics
1.99
article

Unexpected STEVE Observations at High Latitude During Quiet Geomagnetic Conditions

E. Donovan, V. A. Pinto, J. K. Burchill, D. J. Knudsen, Y. Nishimura, L. Kepko, Bea Gallardo‐Lacourt, S. Skone, D. M. Gillies, Jeremy Kuzub, E. Spanswick, D. Chaddock
article en
6 citations

Abstract

Abstract Strong Thermal Emission Velocity Enhancement (STEVE), is a captivating optical phenomenon typically observed in the mid‐latitude ionosphere. This paper presents an intriguing observation of a STEVE event at high‐latitudes, approximately 10 degrees poleward of previously documented observations. This event was recorded in Yellowknife, Canada, by a TREx RGB imager and a citizen scientist. Swarm satellites traversed the latitude of the observation, measuring extreme westwards ion drift velocities exceeding 4 km/s. Such velocities are more typically associated with the subauroral region located at mid‐latitudes, rather than at the high‐latitudes reported here. Significantly, this event occurred without a substorm, which differs from previous STEVE observations. While high‐latitude radars detected fast ionospheric equatorward flows, GOES satellite did not record any injections. These observations suggest that the inner magnetosphere is highly inflated. This unique case study raises new questions surrounding subauroral dynamics and the influence of magnetospheric configurations on ionospheric responses.

Geophysical Research LettersVol. 51(19)
Universidad de Santiago de Chile (CL), Boston University (US), Goddard Space Flight Center (US), University of Calgary (CA), University of America (US), National Aeronautics and Space Administration (US), Catholic University of America (US), Mount Royal University (CA)
National Aeronautics and Space Administration, Agencia Nacional de Investigación y Desarrollo, Canadian Space Agency, Departamento de Investigaciones Científicas y Tecnológicas, Universidad de Santiago de Chile, Air Force Office of Scientific Research
Life below water
Openalex Percentile: Top 14%
Ionosphere and magnetosphere dynamics
1.99
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