Investigation of Precursors in VLF Subionospheric Signals Related to Strong Earthquakes (M > 7) in Western China and Possible Explanations

Earthquakes may disturb the lower ionosphere through various coupling mechanisms during their seismogenic and coseismic periods. The VLF signal radiated from ground-based transmitters is affected when it passes near the disturbed region above the seismogenic area, and this anomaly can be recorded by...

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Main Authors: Shufan Zhao, Xuhui Shen, Li Liao, Zeren Zhima, Chen Zhou, Zhuangkai Wang, Jing Cui, Hengxin Lu
Format: Article
Language:English
Published: MDPI AG 2020-10-01
Series:Remote Sensing
Subjects:
Online Access:https://www.mdpi.com/2072-4292/12/21/3563
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author Shufan Zhao
Xuhui Shen
Li Liao
Zeren Zhima
Chen Zhou
Zhuangkai Wang
Jing Cui
Hengxin Lu
author_facet Shufan Zhao
Xuhui Shen
Li Liao
Zeren Zhima
Chen Zhou
Zhuangkai Wang
Jing Cui
Hengxin Lu
author_sort Shufan Zhao
collection DOAJ
description Earthquakes may disturb the lower ionosphere through various coupling mechanisms during their seismogenic and coseismic periods. The VLF signal radiated from ground-based transmitters is affected when it passes near the disturbed region above the seismogenic area, and this anomaly can be recorded by ground-based VLF receivers. In this paper, the seismic anomalies before two strong earthquakes (M > 7) that occurred in western China were detected using the ground-based observation of VLF signal; the possible reasons for the anomalies were discussed using full wave simulation. The amplitude of the VLF signals observed by the link between NOV, KHA transmitter, and VLF receivers at Ya’an and Tonghai show obvious anomaly by nighttime fluctuation analysis. The simulated results demonstrate that the anomalies could have been induced by ascending/descending of the bottom height of the ionosphere, caused by depletion/increase in D region electron density. The simulated result also illustrates that terminator time shift could have been induced by descending of the bottom boundary of the ionosphere, which is due to modal interference between different wave modes.
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spelling doaj.art-fbc4d8d75dd54c488e0244af4caa92012023-11-20T19:17:11ZengMDPI AGRemote Sensing2072-42922020-10-011221356310.3390/rs12213563Investigation of Precursors in VLF Subionospheric Signals Related to Strong Earthquakes (M > 7) in Western China and Possible ExplanationsShufan Zhao0Xuhui Shen1Li Liao2Zeren Zhima3Chen Zhou4Zhuangkai Wang5Jing Cui6Hengxin Lu7National Institute of Natural Hazards, Ministry of Emergency Management of China, Beijing 100085, ChinaNational Institute of Natural Hazards, Ministry of Emergency Management of China, Beijing 100085, ChinaInstitute of Geophysics, China Earthquake Administration, Beijing 100081, ChinaNational Institute of Natural Hazards, Ministry of Emergency Management of China, Beijing 100085, ChinaSchool of Electronic Information, Wuhan University, Wuhan 430072, ChinaSchool of Electronic Information, Wuhan University, Wuhan 430072, ChinaNational Institute of Natural Hazards, Ministry of Emergency Management of China, Beijing 100085, ChinaNational Institute of Natural Hazards, Ministry of Emergency Management of China, Beijing 100085, ChinaEarthquakes may disturb the lower ionosphere through various coupling mechanisms during their seismogenic and coseismic periods. The VLF signal radiated from ground-based transmitters is affected when it passes near the disturbed region above the seismogenic area, and this anomaly can be recorded by ground-based VLF receivers. In this paper, the seismic anomalies before two strong earthquakes (M > 7) that occurred in western China were detected using the ground-based observation of VLF signal; the possible reasons for the anomalies were discussed using full wave simulation. The amplitude of the VLF signals observed by the link between NOV, KHA transmitter, and VLF receivers at Ya’an and Tonghai show obvious anomaly by nighttime fluctuation analysis. The simulated results demonstrate that the anomalies could have been induced by ascending/descending of the bottom height of the ionosphere, caused by depletion/increase in D region electron density. The simulated result also illustrates that terminator time shift could have been induced by descending of the bottom boundary of the ionosphere, which is due to modal interference between different wave modes.https://www.mdpi.com/2072-4292/12/21/3563precursory of strong earthquakesVLF radio wavenighttime fluctuationseismic anomaliesionospheric disturbancefull-wave model
spellingShingle Shufan Zhao
Xuhui Shen
Li Liao
Zeren Zhima
Chen Zhou
Zhuangkai Wang
Jing Cui
Hengxin Lu
Investigation of Precursors in VLF Subionospheric Signals Related to Strong Earthquakes (M > 7) in Western China and Possible Explanations
Remote Sensing
precursory of strong earthquakes
VLF radio wave
nighttime fluctuation
seismic anomalies
ionospheric disturbance
full-wave model
title Investigation of Precursors in VLF Subionospheric Signals Related to Strong Earthquakes (M > 7) in Western China and Possible Explanations
title_full Investigation of Precursors in VLF Subionospheric Signals Related to Strong Earthquakes (M > 7) in Western China and Possible Explanations
title_fullStr Investigation of Precursors in VLF Subionospheric Signals Related to Strong Earthquakes (M > 7) in Western China and Possible Explanations
title_full_unstemmed Investigation of Precursors in VLF Subionospheric Signals Related to Strong Earthquakes (M > 7) in Western China and Possible Explanations
title_short Investigation of Precursors in VLF Subionospheric Signals Related to Strong Earthquakes (M > 7) in Western China and Possible Explanations
title_sort investigation of precursors in vlf subionospheric signals related to strong earthquakes m 7 in western china and possible explanations
topic precursory of strong earthquakes
VLF radio wave
nighttime fluctuation
seismic anomalies
ionospheric disturbance
full-wave model
url https://www.mdpi.com/2072-4292/12/21/3563
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