Zobrazeno 1 - 6
of 6
pro vyhledávání: '"E. V. Pomozov"'
Autor:
V. V. Denisenko, M. Y. Boudjada, M. Horn, E. V. Pomozov, H. K. Biernat, K. Schwingenschuh, H. Lammer, G. Prattes, E. Cristea
Publikováno v:
Natural Hazards and Earth System Sciences, Vol 8, Iss 5, Pp 1009-1017 (2008)
The classic approach to calculate the electrostatic field penetration, from the Earth's surface into the ionosphere, is to consider the following equation ∇·(σ·∇Φ)=0 where σ and Φ are the electric conductivity and the potential of the elect
Externí odkaz:
https://doaj.org/article/7406f3ccc4d84de78082bc721378b019
Autor:
E. V. Pomozov
Publikováno v:
Geomagnetism and Aeronomy. 54:127-134
In the used model, the quasistationary electric field in the atmosphere of the Earth is obtained by solving the conductivity equation. The penetration characteristics of the electric field from the Earth’s surface into the ionosphere depend on both
Autor:
G. Stangl, A.V. Kitaev, W. Hausleitner, Helfried K. Biernat, Valery V. Denisenko, M. Ampferer, E. V. Pomozov
Publikováno v:
Journal of Atmospheric and Solar-Terrestrial Physics. 102:341-353
A quasi stationary three dimensional model of electric fields and currents in the conductor that includes the Earth's atmosphere and ionosphere is created. The results of the three dimensional model are simpler regarding interpretation and explanatio
Autor:
Valery V. Denisenko, E. V. Pomozov
Publikováno v:
Geomagnetism and Aeronomy. 51:866-872
A mathematical model has been proposed for describing quasi-stationary atmospheric electric fields with approximate, but fairly accurate allowance for ionospheric conductivity. It is shown that some well-known models of electric field penetration fro
Autor:
Mohammed Y. Boudjada, G. Prattes, Helmut Lammer, M. Horn, Valery V. Denisenko, Helfried K. Biernat, Konrad Schwingenschuh, E. V. Pomozov, E. Cristea
Publikováno v:
Natural Hazards and Earth System Sciences. 8:1009-1017
The classic approach to calculate the electrostatic field penetration, from the Earth's surface into the ionosphere, is to consider the following equation ∇·(σ·∇Φ)=0 where σ and Φ are the electric conductivity and the potential of the elect
Publikováno v:
Geomagnetism and Aeronomy. 49:1275-1277
The spatial distributions of electric fields and currents in the Earth’s atmosphere are calculated. Electric potential distributions typical of substorms and quiet geomagnetic conditions are specified in the ionosphere. The Earth is treated as a pe