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Vestnik KRAUNC. Fiziko-Matematicheskie Nauki, 2023, Volume 45, Number 4, Pages 67–80
DOI: https://doi.org/10.26117/2079-6641-2023-45-4-67-80
(Mi vkam624)
 

PHYSICS

Disturbances in the F2 layer of the ionosphere preceding the onset of earthquakes with $ M\geq 6.0$ in the Kamchatka region

V. V. Bogdanov, A. V. Pavlov

Institute of Cosmophysical Research and Radio Wave Propagation FEB RAS
References:
Abstract: The paper presents an analysis of data from hourly measurements of the critical frequency of the ionospheric F2 layer (foF2), carried out over the time interval 01.07.1968-30.07.1997 at the vertical radio sounding station of the ionosphere PK553 (Paratunka, Kamchatka region) in order to identify seismoionospheric anomalies preceding earthquakes with magnitudes $M \geq 6.0$. During the analysis, 45 earthquakes of corresponding magnitudes were considered, in the preparation zone of which, determined by the Dobrovolsky formula, the PK553 ionospheric station was located. The vertical radio sounding station of the ionosphere MG560 (Stekolny, Magadan region) was chosen as a control station. The procedure for detecting seismic-ionospheric disturbances consisted of a joint analysis of the foF2 critical frequency data measured at the reference and control ionospheric stations for vertical radio sounding of the ionosphere. An ionospheric disturbance recorded at a reference station was considered as a possible ionospheric precursor of earthquakes if the deviation of the reference station's foF2 values from the boundaries of the background range of values was observed under conditions of low geomagnetic activity, while the foF2 values of the control station were within its range of background values. Anomalies in foF2 values of the reference station preceded 20% of the considered seismic events. The quantitative characteristics of ionospheric disturbances were made: the maximum relative deviations of the anomalous foF2 values from the median values and from the boundaries of the background range, the lead time of the ionospheric disturbance at the moment of the earthquake. Empirical dependencies were obtained that connect the epicentral distances of earthquakes and the lead time of ionospheric disturbances at the moment of the onset of earthquakes with their magnitude. The identified disturbances of the critical frequency foF2 may be associated with the processes of preparation of the corresponding earthquakes, i.e. may be possible ionospheric precursors of earthquakes.
Keywords: ионосфера, вертикальное радиозондирование, литосфера, землетрясение, предвестник землетрясений, ionosphere, vertical radio sounding, lithosphere, earthquake, earthquake precursor.
Funding agency Grant number
Ministry of Science and Higher Education of the Russian Federation АААА-А21-121011290003-0
The research was carried out in the framework of realization of the State Task АААА-А21-121011290003-0.
Document Type: Article
UDC: 551.510.535
MSC: Primary 86A10; Secondary 86A15
Language: Russian
Citation: V. V. Bogdanov, A. V. Pavlov, “Disturbances in the F2 layer of the ionosphere preceding the onset of earthquakes with $ M\geq 6.0$ in the Kamchatka region”, Vestnik KRAUNC. Fiz.-Mat. Nauki, 45:4 (2023), 67–80
Citation in format AMSBIB
\Bibitem{BogPav23}
\by V.~V.~Bogdanov, A.~V.~Pavlov
\paper Disturbances in the F2 layer of the ionosphere preceding the onset of earthquakes with $ M\geq 6.0$ in the Kamchatka region
\jour Vestnik KRAUNC. Fiz.-Mat. Nauki
\yr 2023
\vol 45
\issue 4
\pages 67--80
\mathnet{http://mi.mathnet.ru/vkam624}
\crossref{https://doi.org/10.26117/2079-6641-2023-45-4-67-80}
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