| Autor: |
Shrivastava MN; Department of Geological Sciences, Universidad Catolica del Norte, Antofagasta, Chile. mahesh.shrivastava@ucn.cl.; National Research Center for Integrated Natural Disaster Management, Santiago, Chile. mahesh.shrivastava@ucn.cl., Maurya AK; Department of Physics, Doon University, Dehradun, India., Gonzalez G; Department of Geological Sciences, Universidad Catolica del Norte, Antofagasta, Chile.; National Research Center for Integrated Natural Disaster Management, Santiago, Chile., Sunil PS; Department of Marine Geology and Geophysics, School of Marine Sciences, Cochin University of Science and Technology, Kochi, India., Gonzalez J; National Research Center for Integrated Natural Disaster Management, Santiago, Chile.; Department of Civil Engineering, Universidad Catolica de la Santísima Concepcion, Concepcion, Chile., Salazar P; Department of Geological Sciences, Universidad Catolica del Norte, Antofagasta, Chile.; National Research Center for Integrated Natural Disaster Management, Santiago, Chile., Aranguiz R; National Research Center for Integrated Natural Disaster Management, Santiago, Chile.; Department of Civil Engineering, Universidad Catolica de la Santísima Concepcion, Concepcion, Chile. |
| Abstrakt: |
To unravel the relationship between earthquake and tsunami using ionospheric total electron content (TEC) changes, we analyzed two Chilean tsunamigenic subduction earthquakes: the 2014 Pisagua M w 8.1 and the 2015 Illapel M w 8.3. During the Pisagua earthquake, the TEC changes were detected at the GPS sites located to the north and south of the earthquake epicenter, whereas during the Illapel earthquake, we registered the changes only in the northward direction. Tide-gauge sites mimicked the propagation direction of tsunami waves similar to the TEC change pattern during both earthquakes. The TEC changes were represented by three signals. The initial weaker signal correlated well with Acoustic Rayleigh wave (AW Rayleigh ), while the following stronger perturbation was interpreted to be caused by Acoustic Gravity wave (AGW epi ) and Internal Gravity wave (IGW tsuna ) induced by earthquakes and subsequent tsunamis respectively. Inevitably, TEC changes can be utilized to evaluate earthquake occurrence and tsunami propagation within a framework of multi-parameter early warning systems. |
