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  5. Analysis of Swarm Satellite Magnetic Field Data Before the 2016 Ecuador (Mw = 7.8) Earthquake Based on Non-negative Matrix Factorization
 
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Analysis of Swarm Satellite Magnetic Field Data Before the 2016 Ecuador (Mw = 7.8) Earthquake Based on Non-negative Matrix Factorization

Author(s)
Zhu, Kaiguang  
College of Instrumentation and Electrical Engineering, Jilin University, Changchun, China  
Fan, Mengxuan  
College of Instrumentation and Electrical Engineering, Jilin University, Changchun, China  
He, Xiaodan  
College of Instrumentation and Electrical Engineering, Jilin University, Changchun, China  
Marchetti, Dedalo  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma2, Roma, Italia  
Li, Kaiyan  
College of Instrumentation and Electrical Engineering, Jilin University, Changchun, China  
Yu, Zining  
College of Instrumentation and Electrical Engineering, Jilin University, Changchun, China  
Chi, Chengquan  
College of Instrumentation and Electrical Engineering, Jilin University, Changchun, China  
Sun, Huihui  
College of Instrumentation and Electrical Engineering, Jilin University, Changchun, China  
Cheng, Yuqi  
College of Instrumentation and Electrical Engineering, Jilin University, Changchun, China  
Language
English
Obiettivo Specifico
7T. Variazioni delle caratteristiche crostali e "precursori"
Status
Published
JCR Journal
JCR Journal
Peer review journal
Yes
Journal
Frontiers in Earth Science  
Issue/vol(year)
/9 (2021)
Electronic ISSN
2296-6463
Publisher
Frontiers Media S.A.
Pages (printed)
621976
Date Issued
April 15, 2021
DOI
10.3389/feart.2021.621976
Alternative Location
https://www.frontiersin.org/articles/10.3389/feart.2021.621976/full
URI
https://www.earth-prints.org/handle/2122/14877
Subjects
04.05. Geomagnetism  
01.02. Ionosphere  
Subjects

Ecuador earthquake

cumulative number of ...

Swarm satellites magn...

non-negative matrix f...

Abstract
In this paper, based on non-negative matrix factorization (NMF), we analyzed the ionosphere magnetic field data of the Swarm Alpha satellite before the 2016 (Mw = 7. 8) Ecuador earthquake (April 16, 0.35°N, 79.93°W), including the whole data collected under quiet and disturbed geomagnetic conditions. The data from each track were decomposed into basis features and their corresponding weights. We found that the energy and entropy of one of the weight components were more concentrated inside the earthquake-sensitive area, which meant that this weight component was more likely to reflect the activity inside the earthquake-sensitive area. We focused on this weight component and used five times the root mean square (RMS) to extract the anomalies. We found that for this weight component, the cumulative number of tracks, which had anomalies inside the earthquake-sensitive area, showed accelerated growth before the Ecuador earthquake and recovered to linear growth after the earthquake. To verify that the accelerated cumulative anomaly was possibly associated with the earthquake, we excluded the influence of the geomagnetic activity and plasma bubble. Through the random earthquake study and low-seismicity period study, we found that the accelerated cumulative anomaly was not obtained by chance. Moreover, we observed that the cumulative Benioff strain S, which reflected the lithosphere activity, had acceleration behavior similar to the accelerated cumulative anomaly of the ionosphere magnetic field, which suggested that the anomaly that we obtained was possibly associated with the Ecuador earthquake and could be described by one of the Lithosphere–Atmosphere–Ionosphere Coupling (LAIC) models.
Sponsors
This research was supported by the National Natural Science Foundation of China under Grant No. 41974084 and the International Cooperation Project of Department of Science and Technology of Jilin Province No. 20200801036GH.
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