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[OI] 557.7 nm airglow during seismic events in the Baikal rift zone

[OI] 557.7 nm airglow during seismic events in the Baikal rift zone 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. http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Atmospheric and Oceanic Optics Springer Journals

[OI] 557.7 nm airglow during seismic events in the Baikal rift zone

Atmospheric and Oceanic Optics , Volume 30 (3) – Jun 15, 2017

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References (21)

Publisher
Springer Journals
Copyright
Copyright © 2017 by Pleiades Publishing, Ltd.
Subject
Physics; Optics, Lasers, Photonics, Optical Devices
ISSN
1024-8560
eISSN
2070-0393
DOI
10.1134/S1024856017030113
Publisher site
See Article on Publisher Site

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.

Journal

Atmospheric and Oceanic OpticsSpringer Journals

Published: Jun 15, 2017

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