@Article{JoshiSripKumaKher:2018:SiDeSe,
author = "Joshi, Lalit Mohan and Sripathi, Samireddipelle and Kumar, Muppidi
Ravi and Kherani, Esfhan Alam",
affiliation = "{Indian Institute of Geomagnetism} and {Indian Institute of
Geomagnetism} and {Indian Institute of Geomagnetism} and
{Instituto Nacional de Pesquisas Espaciais (INPE)}",
title = "Simulating the dependence of seismo-ionospheric coupling on the
magnetic field inclination",
journal = "Annales Geophysicae",
year = "2018",
volume = "36",
number = "1",
pages = "25--35",
month = "Jan.",
keywords = "Atmospheric composition and structure (pressure density and
temperature), history of geophysics (atmospheric sciences),
ionosphere (ionosphere-atmosphere interactions).",
abstract = "Infrasound generated during a seismic event upon reaching the
ionospheric heights possesses the ability to perturb the
ionosphere. Detailed modelling investigation considering 1-D
dissipative linear dynamics, however, indicates that the magnitude
of ionospheric perturbation strongly depends on the magnetic field
inclination. Physics-based SAMI2 model codes have been utilized to
simulate the ionosphere perturbations that are generated due to
the action of the vertical wind perturbations associated with the
seismic infrasound. The propagation of the seismic energy and the
vertical wind perturbations associated with the infrasound in the
model has been considered to be symmetric about the epicentre in
the north-south directions. Ionospheric response to the infrasound
wind, however, has been highly asymmetric in the model simulation
in the north-south directions. This strong asymmetry is related to
the variation in the inclination of the Earth's magnetic field
north and south of the epicentre. Ionospheric monitoring generally
provides an efficient tool to infer the crustal propagation of the
seismic energy. However, the results presented in this paper
indicate that the mapping between the crustal process and the
ionospheric response is not a linear one. These results also imply
that the lithospheric behaviour during a seismic event over a wide
zone in low latitudes can be estimated through ionospheric imaging
only after factoring in the magnetic field geometry.",
doi = "10.5194/angeo-36-25-2018",
url = "http://dx.doi.org/10.5194/angeo-36-25-2018",
issn = "0992-7689",
language = "en",
targetfile = "joshi_simulating.pdf",
urlaccessdate = "27 abr. 2024"
}