4.6 Article

Locating surface deformation induced by earthquakes using GPS, GLONASS and Galileo ionospheric sounding from a single station

Journal

ADVANCES IN SPACE RESEARCH
Volume 68, Issue 8, Pages 3403-3416

Publisher

ELSEVIER SCI LTD
DOI: 10.1016/j.asr.2021.06.011

Keywords

GNSS; TEC; Earthquake monitoring; Ionosphere seismology; Single-station; Galileo

Funding

  1. French Space Agency CNES (Centre National d'Etudes Spatiales)
  2. Universite Cote d'Azur Investissement d'Avenir Idex project - ANR (Agence Nationale de la Recherche)
  3. ANR JCJC E-POST [ANR-14-CE03-002-01JCJC EPOST]
  4. European Research Council (ERC) [805256]
  5. Observatoire de la Cote d'Azur
  6. European Research Council (ERC) [805256] Funding Source: European Research Council (ERC)

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The study evaluates the capability of a single GNSS station to constrain the origin location of coseismic ionospheric disturbances (CID) through observations of Total Electron Content (TEC). It confirms that increasing the number of monitoring satellites helps in resolving CID origins. By using TEC data from earthquakes of different moment magnitudes, the research shows that a well-placed multi-GNSS station can accurately retrieve the origin of CID with a high level of precision.
Monitoring earthquakes to rapidly forecast their consequences remains a challenging task, especially in areas far from seismic and geodetic networks. Large and shallow earthquakes induce disturbances in the ionospheric Total Electron Content (TEC). These disturbances are commonly detected using Global Navigation Satellite Systems (GNSS) stations that can sound the ionosphere at great distances. To address this instrumentation sparsity issue, we assess a single GNSS station's ability to constrain the origin location of a coseismic ionospheric disturbance (CID) using observations of TEC. We develop a grid-search method that explores different trial origins (i.e. source locations) to determine which synthetic CID signal best matches the observed TEC time series. We confirm that a larger number of monitoring satellites enhances the opportunity to have the favorable geometrical coverage of satellites needed to resolve CID origins. We use TEC data acquired during two earthquakes having different moment magnitudes: a Mw 7.1 from Turkey and a Mw 7.8 from New Zealand. Using a well-placed multi-GNSS station we are able to retrieve the CID origin with an accuracy of 50 km and a theoretical precision of the same order. We conclude that a very sparse network of multi-GNSS stations can provide an independent estimate of the spatial distribution of large scale coseismic motions, including offshore areas 200-300 km from the coastline. (C) 2021 COSPAR. Published by Elsevier B.V. All rights reserved.

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