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  5. Integrating Pre-Earthquake Signatures From Different Precursor Tools
 
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Integrating Pre-Earthquake Signatures From Different Precursor Tools

Author(s)
Ghamry, Essam  
Mohamed, Emad K  
Abdalzaher, Mohamed S.  
Elwekeil, Mohamed  
Marchetti, Dedalo  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma2, Roma, Italia  
De Santis, Angelo  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma2, Roma, Italia  
Hegy, Mostafa  
Yoshikawa, Akimasa  
Fathy, Adel  
Language
English
Obiettivo Specifico
7T. Variazioni delle caratteristiche crostali e "precursori"
Status
Published
JCR Journal
JCR Journal
Peer review journal
Yes
Journal
IEEE Access  
Issue/vol(year)
/9 (2021)
Publisher
IEEE
Pages (printed)
33268-33283
Date Issued
2021
DOI
10.1109/ACCESS.2021.3060348
URI
https://www.earth-prints.org/handle/2122/15578
Abstract
Potential earthquake precursors include, among others, electromagnetic fields, gas emissions, Land Surface Temperature (LST), Sea Surface Temperature (SST), and Surface Air Temperature (SAT) anomalies. These observables have been individually studied, before earthquakes, by many researchers. The ionospheric studies concerning earthquakes (EQs) using magnetic data from Low Earth Orbit (LEO) satellites are increasingly being used to detect ionospheric anomalies before large EQs. Also, LST, SST, and SAT values retrieved from Moderate Resolution Imaging Spectroradiometer (MODIS) Terra and Aqua satellites and Modern-Era Retrospective analysis for Research and Applications Version 2 (MERRA-2) are considered as physical precursors before EQs. In this work, we jointly analyze magnetic, MODIS, and MERRA-2 data in space and time around the epicenters before the selected EQs in Mexico, Japan, Chile, and Indonesia. Our analyses present interesting findings where anomalies in temperature and magnetic field, preceding the considered EQs, are confirmed through different methods. Particularly, we utilize the Fast Fourier Transform (FFT) and the Discrete Cosine Transform (DCT) for analyzing magnetic data over the designated EQs regions. We use the magnetic data acquired by Swarm satellites in the top side ionosphere along with MODIS and MERRA-2. Five case studies are described to prove the effectiveness of our analyses. Precursory anomalies were observed using these methods in different anomalous days from the considered four regions of interest around the epicenter. It is concluded that these methods could be effective and reliable in detecting anomalies preceding the upcoming EQs.
Type
article
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Ghamry et al. 2021_Integrating_Pre-Earthquake_Signatures_From_Different_Precursor_Tools.pdf

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Open Access published article
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3.59 MB

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