Virtual array beamforming of GPS TEC observations of coseismic ionospheric disturbances near the Geomagnetic South Pole triggered by teleseismic megathrusts

We identified coseismic ionospheric disturbances (CID) in Antarctica generated by the 2010 Maule and the 2011 Tohoku-Oki earthquakes analyzing total electron content (TEC) data with a modified beamforming technique. Beamforming in Antarctica, however, is not straightforward due to the effects of arr...

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Bibliographic Details
Published in:Journal of Geophysical Research: Space Physics
Main Authors: Gõmez, Demián, Smalley, Robert, Langston, Charles A., Wilson, Terry J., Bevis, Michael, Dalziel, Ian W.D., Kendrick, Eric C., Konfal, Stephanie A.
Format: Text
Language:unknown
Published: University of Memphis Digital Commons 2015
Subjects:
Antarctica
beamforming
coseismic ionospheric disturbances
ionosphere
total electron content
virtual array
Geophysics and Seismology
South Pole
Antarc*
South pole
Online Access:https://digitalcommons.memphis.edu/facpubs/1449
https://doi.org/10.1002/2015JA021725
Description
Summary:We identified coseismic ionospheric disturbances (CID) in Antarctica generated by the 2010 Maule and the 2011 Tohoku-Oki earthquakes analyzing total electron content (TEC) data with a modified beamforming technique. Beamforming in Antarctica, however, is not straightforward due to the effects of array deformation and atmospheric neutral wave-ionospheric plasma coupling. We take these effects into account and present a method to invert for the seismically generated acoustic wave using TEC observations. The back azimuths, speeds, and waveforms obtained by the beamform are in excellent agreement with the hypothesis that the TEC signals are generated by the passage of Rayleigh waves from the Maule and Tohoku-Oki earthquakes. The Tohoku-Oki earthquake is ~12,500 km from Antarctica, making this the farthest observation of CIDs to date using GPS.

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