Acoustic waves generated from seismic surface waves: propagation properties determined from Doppler sounding observations and normal-mode modelling

By J. Artru, T. Farges, Philippe Lognonné. 2004

209 citations recorded by the source corpus.

Subfields: Astronomy and Astrophysics, Geophysics

View Paper: https://www.semanticscholar.org/paper/632512ae69fa15d8b5cf13ee3909426c42ae5b11

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Citations in the corpus

Detection and modeling of Rayleigh wave induced patterns in the ionosphere (2011, background): “…a pressure seismic surface wave with a velocity of 1 mm/s on the ground, corresponding to teleseismic surface waves generated by a shallow earthquake with magnitude 8, reaches the maximum of ionization (F2 ionospheric peak) with many tens to a few hundreds of meters per second [Artru et al., 2004].”
Directivity and apparent velocity of the coseismic ionospheric disturbances observed with a dense GPS array (2005, background): “This might be the Denali case [4], where GPS points are > 2000 km apart from the epicenter, and other cases reported recently using Doppler sounding [15]”
GNSS ionospheric seismology: Recent observation evidences and characteristics (2015, background): “Consequently, a new perspective of earthquake effects is provided by the characteristic analysis of seismic ionospheric disturbance estimated through observing the ionosphere (Najita and Yuen, 1979; Tanaka et al., 1984; Artru et al., 2004; Jin et al., 2010; Occhipinti et al., 2010).”
Ionospheric detection of gravity waves induced by tsunamis (2005, unknown): “Ionospheric oscillations induced in the wake of Rayleigh wave propagation is indeed systematically observed using ground-based Doppler sounding, for magnitudes greater than 6.5 (Artru et al. 2004).”
Scientific goals for the observation of Venus by VIRTIS on ESA/Venus Express mission (2007, background): “, 1985; Calais and Minster, 1995) and, far from the event, above seismic surface waves (Ducic et al., 2003; Artru et al., 2004; Garcia et al., 2005a).”
Giant ionospheric disturbances excited by the M9.3 Sumatra earthquake of 26 December 2004 (2006, background): “…that transient disturbances can occur in the ionosphere as a result of big earthquakes [Bolt, 1964; Leonard and Barnes, 1965; Davies and Baker, 1965; Row, 1966, 1967; Yuen et al., 1969; Tanaka et al., 1984; Calais and Minster, 1995; Afraimovich et al., 2001, 2002a, 2002b; Artru et al., 2001, 2004].”
From Sumatra 2004 to Tohoku‐Oki 2011: The systematic GPS detection of the ionospheric signature induced by tsunamigenic earthquakes (2013, background): “…the ground vertical displacement induced by surface waves, allows to image the radiation pattern of the seismic tensor in the near field [Rolland et al., 2011a], and it is routinely observed by Doppler sounders in the far field for earthquakes with a magnitude bigger than 6.5 [Artru et al., 2004].”