[OI] 557.7 nm airglow during seismic events in the Baikal rift zone
- Authors: Mikhalev A.V.1
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Affiliations:
- Institute of Solar-Terrestrial Physics, Siberian Branch
- Issue: Vol 30, No 3 (2017)
- Pages: 243-247
- Section: Acoustooptical and Radiooptical Methods for Environmental Studies
- URL: https://journals.rcsi.science/1024-8560/article/view/188066
- DOI: https://doi.org/10.1134/S1024856017030113
- ID: 188066
Cite item
Abstract
Atomic oxygen [OI] 557.7-nm atmospheric emission (airglow altitudes of 85–115 km) during earthquakes (EQ) with a magnitude of M ≥ 5, occurred in the Baikal rift zone in 2014–2016, is studied. Variations in this emission are analyzed; higher values of mean nighttime intensities of this emission on several days before an EQ in comparison with subsequent days are revealed. A possible explanation of these variations during EQs is given.
Keywords
About the authors
A. V. Mikhalev
Institute of Solar-Terrestrial Physics, Siberian Branch
Author for correspondence.
Email: mikhalev@iszf.irk.ru
Russian Federation, Irkutsk, 664033
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