Diagnosis of the high-latitude ionosphere and spatio-temporal dynamics of auroral precipitation
- Authors: Kozelov B.V.1, Vorobyov V.G.1, Titova E.E.1, Popova T.A.1
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Affiliations:
- Polar Geophysical Institute
- Issue: Vol 88, No 3 (2024)
- Pages: 460-466
- Section: Physics of Auroral Phenomena
- URL: https://cardiosomatics.ru/0367-6765/article/view/654735
- DOI: https://doi.org/10.31857/S0367676524030162
- EDN: https://elibrary.ru/QLKLAC
- ID: 654735
Cite item
Abstract
Using high-latitude observations by the Polar Geophysical Institute, the development of a typical auroral substorm on September 13, 2013, is traced. The event, according to satellite data, is linked to solar wind parameters, physical magnetospheric domains, and boundaries. The characteristics of the spatial structure of polar auroras (scaling indices, anisotropy) have been determined for typical auroral structures (quiet and rayed arcs, breakup, pulsating bands, omega structures).
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About the authors
B. V. Kozelov
Polar Geophysical Institute
Author for correspondence.
Email: boris.kozelov@gmail.com
Russian Federation, Apatity
V. G. Vorobyov
Polar Geophysical Institute
Email: boris.kozelov@gmail.com
Russian Federation, Apatity
E. E. Titova
Polar Geophysical Institute
Email: boris.kozelov@gmail.com
Russian Federation, Apatity
T. A. Popova
Polar Geophysical Institute
Email: boris.kozelov@gmail.com
Russian Federation, Apatity
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