Disturbances in the F2 region critical frequency before the earthquake of September 11, 2008 off the coast of Hokkaido, Japan, and during a moderate magnetic storm based on data from ground-based vertical ionosphere sounding stations
- Авторы: Legen’ka A.D.1, Hegai V.V.1, Kim V.P.1
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Учреждения:
- Pushkov Institute of Terrestrial Magnetism, Ionosphere and Radio Wave Propagation
- Выпуск: Том 56, № 3 (2016)
- Страницы: 331-341
- Раздел: Article
- URL: https://journal-vniispk.ru/0016-7932/article/view/155663
- DOI: https://doi.org/10.1134/S0016793216030129
- ID: 155663
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Аннотация
Based on data from ground-based vertical sounding stations, the behaviors of the ionosphere F region before a strong M 6.8 earthquake off the coast of Hokkaido, Japan, and during the moderate magnetic storm before this earthquake are compared. It was found that the critical frequency of the ionosphere F region (foF2) above the Wakkanai ground-based ionosphere vertical sounding station, which was located in the preparation zone of this earthquake, suffered a long-term disturbance of slightly more than an hour nearly half a day before the earthquake. The magnitude of earthquake-induced disturbance is comparable to that caused by a magnetic storm.
Об авторах
A. Legen’ka
Pushkov Institute of Terrestrial Magnetism, Ionosphere and Radio Wave Propagation
Автор, ответственный за переписку.
Email: leg@izmiran.ru
Россия, Troitsk, Moscow, 142190
V. Hegai
Pushkov Institute of Terrestrial Magnetism, Ionosphere and Radio Wave Propagation
Email: leg@izmiran.ru
Россия, Troitsk, Moscow, 142190
V. Kim
Pushkov Institute of Terrestrial Magnetism, Ionosphere and Radio Wave Propagation
Email: leg@izmiran.ru
Россия, Troitsk, Moscow, 142190
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