Decrease of the electric field penetration into the ionosphere due to low conductivity at the near ground atmospheric layer

It is well known that lithospheric electromagnetic emissions are generated before earthquakes occurrence. In our study, we consider the physical penetration mechanism of the electric field from the Earth's surface, through the atmosphere-ionosphere layers, and until its detection in space by...

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Main Authors: M. Ampferer, V. V. Denisenko, W. Hausleitner, S. Krauss, G. Stangl, M. Y. Boudjada, H. K. Biernat
Format: Article
Language:English
Published: Copernicus Publications 2010-03-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/28/779/2010/angeo-28-779-2010.pdf
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author M. Ampferer
V. V. Denisenko
V. V. Denisenko
W. Hausleitner
S. Krauss
G. Stangl
G. Stangl
M. Y. Boudjada
H. K. Biernat
H. K. Biernat
H. K. Biernat
author_facet M. Ampferer
V. V. Denisenko
V. V. Denisenko
W. Hausleitner
S. Krauss
G. Stangl
G. Stangl
M. Y. Boudjada
H. K. Biernat
H. K. Biernat
H. K. Biernat
author_sort M. Ampferer
collection DOAJ
description It is well known that lithospheric electromagnetic emissions are generated before earthquakes occurrence. In our study, we consider the physical penetration mechanism of the electric field from the Earth's surface, through the atmosphere-ionosphere layers, and until its detection in space by satellites. A simplified approach is investigated using the electric conductivity equation, i.e., ∇ˆσ·∇Φ)=0 in the case of a vertical inclination of the geomagnetic field lines. Particular interest is given to the conductivity profile near the ground and the electric field distribution at the Earth's surface. Our results are discussed and compared to the models of Pulinets et al. (2003) and Denisenko et al. (2008). It is shown that the near ground atmospheric layer with low conductivity decreases the electric field penetration into the ionosphere. The model calculations have demonstrated that the electric field of lithospheric origin is too weak to be observed at satellite altitudes.
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spelling doaj.art-c962b83fd46b4427a575daa08dbf13e02022-12-21T17:31:12ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762010-03-012877978710.5194/angeo-28-779-2010Decrease of the electric field penetration into the ionosphere due to low conductivity at the near ground atmospheric layerM. Ampferer0V. V. Denisenko1V. V. Denisenko2W. Hausleitner3S. Krauss4G. Stangl5G. Stangl6M. Y. Boudjada7H. K. Biernat8H. K. Biernat9H. K. Biernat10Institute of Physics, Department of Geophysics, Astrophysics and Meteorology, Karl-Franzens-University Graz, AustriaInstitute of Computational Modelling, Russian Academy of Sciences, Siberian Branch, Krasnoyarsk, RussiaSiberian Federal University, Krasnoyarsk, RussiaSpace Research Institute, Austrian Academy of Sciences, Graz, AustriaSpace Research Institute, Austrian Academy of Sciences, Graz, AustriaSpace Research Institute, Austrian Academy of Sciences, Graz, AustriaFederal Office of Metrology and Surveying, Vienna, AustriaSpace Research Institute, Austrian Academy of Sciences, Graz, AustriaInstitute of Physics, Department of Geophysics, Astrophysics and Meteorology, Karl-Franzens-University Graz, AustriaSpace Research Institute, Austrian Academy of Sciences, Graz, AustriaInstitute of Physics, Department of Theoretical Physics, Karl-Franzens-University Graz, AustriaIt is well known that lithospheric electromagnetic emissions are generated before earthquakes occurrence. In our study, we consider the physical penetration mechanism of the electric field from the Earth's surface, through the atmosphere-ionosphere layers, and until its detection in space by satellites. A simplified approach is investigated using the electric conductivity equation, i.e., ∇ˆσ·∇Φ)=0 in the case of a vertical inclination of the geomagnetic field lines. Particular interest is given to the conductivity profile near the ground and the electric field distribution at the Earth's surface. Our results are discussed and compared to the models of Pulinets et al. (2003) and Denisenko et al. (2008). It is shown that the near ground atmospheric layer with low conductivity decreases the electric field penetration into the ionosphere. The model calculations have demonstrated that the electric field of lithospheric origin is too weak to be observed at satellite altitudes.https://www.ann-geophys.net/28/779/2010/angeo-28-779-2010.pdf
spellingShingle M. Ampferer
V. V. Denisenko
V. V. Denisenko
W. Hausleitner
S. Krauss
G. Stangl
G. Stangl
M. Y. Boudjada
H. K. Biernat
H. K. Biernat
H. K. Biernat
Decrease of the electric field penetration into the ionosphere due to low conductivity at the near ground atmospheric layer
Annales Geophysicae
title Decrease of the electric field penetration into the ionosphere due to low conductivity at the near ground atmospheric layer
title_full Decrease of the electric field penetration into the ionosphere due to low conductivity at the near ground atmospheric layer
title_fullStr Decrease of the electric field penetration into the ionosphere due to low conductivity at the near ground atmospheric layer
title_full_unstemmed Decrease of the electric field penetration into the ionosphere due to low conductivity at the near ground atmospheric layer
title_short Decrease of the electric field penetration into the ionosphere due to low conductivity at the near ground atmospheric layer
title_sort decrease of the electric field penetration into the ionosphere due to low conductivity at the near ground atmospheric layer
url https://www.ann-geophys.net/28/779/2010/angeo-28-779-2010.pdf
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