Use of the index of TEC vertical variation disturbance in studying ionospheric effects of the Chelyabinsk meteorite
- Authors: Voeykov S.V.1, Berngardt O.I.1, Shestakov N.V.2,3
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Affiliations:
- Institute of Solar–Terrestrial Physics, Siberian Branch
- Far East Federal University
- Institute of Applied Mathematics, Far East Branch
- Issue: Vol 56, No 2 (2016)
- Pages: 219-228
- Section: Article
- URL: https://journals.rcsi.science/0016-7932/article/view/155604
- DOI: https://doi.org/10.1134/S0016793216020122
- ID: 155604
Cite item
Abstract
The results of an analysis of the ionospheric effects accompanying fall of the Chelyabinsk meteorite on February 15, 2013 are presented using a method of calculating the index of the disturbance of total electron content vertical variations (Wtec) according to data from the GPS receiver network. A substantial increase (by a factor of 2–3) in the Wtec index with a duration of ~1.5 h was observed in the studied region after the main height explosion accompanying the meteorite fall at 0320 UT. The ionospheric response in Wtec was most significant statistically registered at the radio rays “receiver–satellite” for the GPS located southward from the place of explosion.
About the authors
S. V. Voeykov
Institute of Solar–Terrestrial Physics, Siberian Branch
Author for correspondence.
Email: serg3108@iszf.irk.ru
Russian Federation, ul. Lermontova 126a, Irkutsk, 664033
O. I. Berngardt
Institute of Solar–Terrestrial Physics, Siberian Branch
Email: serg3108@iszf.irk.ru
Russian Federation, ul. Lermontova 126a, Irkutsk, 664033
N. V. Shestakov
Far East Federal University; Institute of Applied Mathematics, Far East Branch
Email: serg3108@iszf.irk.ru
Russian Federation, ul. Sukhanova 8, Vladivostok, 690600; ul. Radio 7, Vladivostok, 690041
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