Ionospheric remote sensing of the Denali Earthquake Rayleigh surface waves

  • Vesna Ducic
    Département de Géophysique Spatiale et Planétaire, UMR7096 Institut de Physique du Globe de Paris France
  • Juliette Artru
    Seismological Laboratory California Institute of Technology Pasadena California USA
  • Philippe Lognonné
    Département de Géophysique Spatiale et Planétaire, UMR7096 Institut de Physique du Globe de Paris France

書誌事項

公開日
2003-09
権利情報
  • http://onlinelibrary.wiley.com/termsAndConditions#vor
DOI
  • 10.1029/2003gl017812
公開者
American Geophysical Union (AGU)

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説明

<jats:p>Using the Global Positioning System, we have detected ionospheric disturbances associated with the long‐period Rayleigh waves from the 2002 Denali earthquake (M<jats:sub>s</jats:sub> = 7.9). The dense California GPS networks allowed us to map the ionospheric perturbations and to compute the group velocity with a high spatial resolution above the Pacific coasts. Due to a low sampling rate, a large error in the velocity determination remains. Nonetheless, it demonstrates that bi‐static remote sensing measurements of seismic waves with GPS networks can be performed. Monostatic measurements with a dedicated satellite could possibly be used to record in the ionosphere surface waves originating from large earthquakes. Such a space‐based remote sensing of the local group velocity of Rayleigh surface waves would effectively complement the seismic networks for high‐resolution global tomography of the Earth's lithosphere.</jats:p>

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