TY - JOUR
T1 - Integrating Pre-Earthquake Signatures from Different Precursor Tools
AU - Ghamry, Essam
AU - Mohamed, Emad K.
AU - Abdalzaher, Mohamed S.
AU - Elwekeil, Mohamed
AU - Marchetti, Dedalo
AU - De Santis, Angelo
AU - Hegy, Mostafa
AU - Yoshikawa, Akimasa
AU - Fathy, Adel
N1 - Funding Information:
This work was supported by JSPS KAKENHI under Grant JP20H01961 and Grant JP15H05815.
Funding Information:
The authors thank the European Space Agency (ESA) for providing the Swarm data which can be accessed freely from the Swarm website: ftp://swarm-diss.eo.esa.int. They also thank USGS organization for providing MODIS V6 product data. The MODIS data can be downloaded from https://earthexplorer.usgs.gov and https://lpdaacsvc.cr.usgs. gov. They also thank LIMADOU-Science project funded by Italian Space Agency. This work was supported by JSPS KAKENHI under Grant JP20H01961 and Grant JP15H05815.
Publisher Copyright:
© 2013 IEEE.
PY - 2021
Y1 - 2021
N2 - 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.
AB - 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.
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U2 - 10.1109/ACCESS.2021.3060348
DO - 10.1109/ACCESS.2021.3060348
M3 - Article
AN - SCOPUS:85101735395
SN - 2169-3536
VL - 9
SP - 33268
EP - 33283
JO - IEEE Access
JF - IEEE Access
M1 - 9360318
ER -