Propagation of tsunami‐driven gravity waves into the thermosphere and ionosphere

By M. Hickey, Gerald Schubert, Richard L. Walterscheid. 2009

147 citations recorded by the source corpus.

Subfields: Astronomy and Astrophysics, Geophysics

View Paper: https://www.semanticscholar.org/paper/9fd5c36388216c53bb206a15257d793758190bb8

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Citations in the corpus

GNSS ionospheric seismology: Recent observation evidences and characteristics (2015, methodology): “D) modeling on the tsunami– atmosphere–ionosphere coupling should be done with the viscosity and thermal conduction as already tested in a 1D case by Hickey et al. (2009).”
Ionospheric gravity waves detected offshore Hawaii after tsunamis (2010, background): “[2008] and by Hickey et al. [2009]. [5] We present here three occurrences of far‐field ionospheric perturbations offshore Hawaii, following three significant tsunami events triggered by earthquakes located in three different geographical directions, as shown on Figure 1a:Northwest, theMw8.”
From Sumatra 2004 to Tohoku‐Oki 2011: The systematic GPS detection of the ionospheric signature induced by tsunamigenic earthquakes (2013, background): “Other theoretical works appeared recently to explore the possible detection by airglow monitoring [Hickey et al., 2010] and Over-The-Horizon radar [Coïsson et al., 2011], as well as to calculate the effect of dissipation, nominal viscosity, and thermal conduction [Hickey et al., 2009].”
Detection and modeling of Rayleigh wave induced patterns in the ionosphere (2011, background): “However, none of these methods includes the other source of atmospheric attenuation, such as thermal conduction and the collisions of ions on neutral particles [e.g., Hickey et al., 2009].”
Imaging and modeling the ionospheric airglow response over Hawaii to the tsunami generated by the Tohoku earthquake of 11 March 2011 (2011, background): “Due to the decrease in atmospheric density and the requirement that wave momentum is conserved, the amplitudes of the forced AGWs can reach several kilometers at altitudes where the neutral atmosphere coexists with the plasma in the ionosphere (∼250 km), perturbing the ionosphere through collisions ”
Internal wave coupling processes in Earth's atmosphere (2014, unknown): “The effects of GW dissipation in the thermosphere have recently been a subject of detailed studies employing direct wave simulation models (Hickey et al., 2009, 2010; Walterscheid , 2013; Heale et al., 2014).”