Co-seismic ionospheric disturbances characteristics in different azimuths following the 2022 Mexico earthquake from GNSS observations
Author:
Funder
National Natural Science Foundation of China Project
Publisher
Springer Science and Business Media LLC
Subject
General Earth and Planetary Sciences
Link
https://link.springer.com/content/pdf/10.1007/s10291-023-01564-9.pdf
Reference35 articles.
1. Afraimovich EL, Perevalova NP, Plotnikov AV, Uralov AM (2001) The shock-acoustic waves generated by earthquakes. Ann Geophys 19(4):395–409. https://doi.org/10.5194/angeo-19-395-2001
2. Artru J, Farges T, Lognonne L (2004) Acoustic waves generated from seismic surface waves: propagation properties determined from Doppler sounding observations and normal-mode modelling. Geophys J Int 158(3):1067–1077. https://doi.org/10.1111/j.1365-246X.2004.02377.x
3. Astafyeva E, Heki K (2009) Dependence of waveform of near-field coseismic ionospheric disturbances on focal mechanisms. Earth Planets Space 61:939–943. https://doi.org/10.1186/BF03353206
4. Astafyeva E, Heki K, Vladislav K, Afraimovich E, Shalimov S (2009) Two-mode long-distance propagation of coseismic ionosphere disturbances. J Geophys Res Space Phys 114(A10):A10307. https://doi.org/10.1029/2008ja013853
5. Astafyeva E, Shalimov S, Olshanskaya E, Lognonné P (2013) Ionospheric response to earthquakes of different magnitudes: larger quakes perturb the ionosphere stronger and longer. Geophys Res Lett 40(9):1675–1681. https://doi.org/10.1002/grl.50398
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