@InProceedings{KheraniLognPaulHerb:2009:IoDiOb,
author = "Kherani, E. Alam and Lognonne, L. and Paula, Eurico Rodrigues de
and Herbert, H.",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Institut
de Physique du Globo de Paris} and {Instituto Nacional de
Pesquisas Espaciais (INPE)} and {Institut de Physique du Globo de
Paris}",
title = "The ionospheric disturbances observed prior to sumatra tsunami and
their possible association with pre-tsunami activity",
booktitle = "Proceedings...",
year = "2009",
organization = "Iaga, 2009.",
keywords = "Ionosphere, Acoustic gravity waves, Tsunami.",
abstract = "In this work, we present the results from CHAMP and COSMIC
satellite measurements of neutral density, temperature,
ionospheric density and electromagnetic disturbances in atmosphere
and ionosphere registered before and during few
Earthquakes/Tsunami. Three Sumatra tsunamis, SUM1 (26 Dec 2004,
00:58:53 UT, Mw=9.1, 3.31N, 95.85E), SUM2 (28 Mar 2005, 16:09:36
UT, Mw=8.6, 2.074N, 97.013E) and SUM3 (12 Sep 2007, 11:10:26 UT,
Mw=8.5, 4.52S, 101.37E). For SUM1 and SUM2, CHAMP measurements of
electromagnetic and electron density disturbances in the
ionosphere are analyzed. For SUM3, COSMIC measurements of
atmospheric and ionospheric disturbances are also analyzed. In
first step, disturbances registered during these events are
examined. In particular, their timespatial scale and spectral
distributions are studied. Knowing these aspects, similar
features, though in much reduced magnitudes and possibly in much
slower timescale, are searched in the satellite data prior to
these events. In this way, we could find disturbances which may be
possibly associated with pre-tsunami activities. We also present
computational simulation of possible excitation of disturbances
near Earth's surface and in the atmosphere/ionosphere caused by
tiny rock deformation in the lithosphere prior to an
earthquake/tsunami. In first step, the study pursue an excitation
of acoustic wave in the lithosphere caused by rock deformation,
its propagation in solid Earth up-to Earth's surface and
deposition of momentum and energy at the Earth's surface. In
second step, excitation of neutral waves such as acoustic gravity
waves (AGWs) caused by deposition of momentum/energy and their
propagation in the atmosphere is studied using
thermo-hydro-viscous fluid simulation. In third and final step,
AGWs interaction with ionosphere is studied using
thermo-hydro-magnetic fluid simulation.",
conference-location = "Sopron, Hungary",
conference-year = "23-30 Aug.",
label = "self-archiving-INPE-MCTIC-GOV-BR",
language = "en",
targetfile = "kherani_ionospheric.pdf",
urlaccessdate = "03 maio 2024"
}