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Disturbances in E and F Layers of the Ionosphere Preceding Earthquakes in the Kamchatka Region

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Solar-Terrestrial Relations and Physics of Earthquake Precursors (STRPEP 2023)

Abstract

Anomalous changes in the parameters characterizing the state of the ionospheric layers E and F, observed before the onset of seismic events, can be considered as possible ionospheric precursors of these earthquakes. In this work, according to the data obtained at the ionospheric station of vertical radio sounding, located in Paratunka (\(52.97^\circ \) N, \(158.24^\circ \) E), an analysis of ionospheric disturbances recorded before the onset of earthquakes with magnitude \(M\ge 5.0\) that occurred in the Kamchatka region was carried out. Anomalous values of the limiting reflection frequency foEs, the screening frequency fbEs and the virtual height \(h'Es\) of the sporadic Es layer, as well as the critical frequency foF2 of the F2 layer and the virtual height \(h'F\) of the F layer in the absence of geomagnetic disturbances were considered as possible ionospheric precursors of earthquakes. The predictive efficiency of the anomalous behavior of the complex of considered ionospheric parameters for earthquakes with \(M\ge 5.0\) is estimated.

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Acknowledgments

The work was carried out within the framework of the State task on the topic (2021–2023) “Physical processes in the system of near space and geospheres under solar and lithospheric impact”, registration number AAAA-A21-121011290003-0.

The work was realized by the means of the Common Use Center “North-Eastern Heliogeophysical Center” CKP_558279, USU 351757.

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Correspondence to Aleksey Pavlov .

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Bogdanov, V., Pavlov, A. (2023). Disturbances in E and F Layers of the Ionosphere Preceding Earthquakes in the Kamchatka Region. In: Dmitriev, A., Lichtenberger, J., Mandrikova, O., Nahayo, E. (eds) Solar-Terrestrial Relations and Physics of Earthquake Precursors. STRPEP 2023. Springer Proceedings in Earth and Environmental Sciences. Springer, Cham. https://doi.org/10.1007/978-3-031-50248-4_25

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