Add to ORKG109-113Heating of the ionosphere due to incidence of electromagnetic pulses coming from lightning discharges has been theoretically investigated. The electromagnetic radiation from lightning discharges produces variation in ionizing frequency and effective collision frequency of electrons. The energy gained by the free electrons from the incident electric fields of wide-band electromagnetic pulses from lightning strikes is not instantaneously transferred to the heavy particles in the medium, due to which the electron temperature is raised. Variation of temperature increase has been estimated
Very Low Frequency (VLF 3-30 kHz) receivers are used to monitor the amplitude and phase of signals f...
It is possible to observe and control to a limited extent the changes in characteristic ionospheric ...
The electron temperature changes due to 3, 5 and 430 MHz radio wave heating in the lower ionosphere ...
In this study, the heating of the nighttime lower ionosphere due to electromagnetic radiation in the...
In this study, the heating of the nighttime lower ionosphere due to electromagnetic radiation in the...
A connection between thunderstorms and the ionosphere has been hypothesized since the mid-1920s(1). ...
The lower ionosphere has been heated in a controlled experiment at the Arecibo ionospheric Observato...
93-97The ionospheric temperature in relation with the thunderstorm activity has been studied. The d...
In this paper, Maxwell’s equations are solved for the ionospheric plasma during thunderstorm and lig...
The lower ionosphere influences the propagation of electromagnetic (EM) waves, satellite and also te...
The effect of lightning-induced electromagnetic (EM) waves on electron density (Ne) of the lower ion...
An ionospheric heating experiment has been performed at the Arecibo Observatory using the 43 MHz inc...
thunderstorm-driven electrodynamic coupling between the troposphere, mesosphere, lower ionosphere, a...
286-290Effects of heating of the ionosphere during high power radio wave propagation have been inves...
Thesis (Sc. D.)--Massachusetts Institute of Technology, Dept. of Electrical Engineering and Computer...
Very Low Frequency (VLF 3-30 kHz) receivers are used to monitor the amplitude and phase of signals f...
It is possible to observe and control to a limited extent the changes in characteristic ionospheric ...
The electron temperature changes due to 3, 5 and 430 MHz radio wave heating in the lower ionosphere ...
In this study, the heating of the nighttime lower ionosphere due to electromagnetic radiation in the...
In this study, the heating of the nighttime lower ionosphere due to electromagnetic radiation in the...
A connection between thunderstorms and the ionosphere has been hypothesized since the mid-1920s(1). ...
The lower ionosphere has been heated in a controlled experiment at the Arecibo ionospheric Observato...
93-97The ionospheric temperature in relation with the thunderstorm activity has been studied. The d...
In this paper, Maxwell’s equations are solved for the ionospheric plasma during thunderstorm and lig...
The lower ionosphere influences the propagation of electromagnetic (EM) waves, satellite and also te...
The effect of lightning-induced electromagnetic (EM) waves on electron density (Ne) of the lower ion...
An ionospheric heating experiment has been performed at the Arecibo Observatory using the 43 MHz inc...
thunderstorm-driven electrodynamic coupling between the troposphere, mesosphere, lower ionosphere, a...
286-290Effects of heating of the ionosphere during high power radio wave propagation have been inves...
Thesis (Sc. D.)--Massachusetts Institute of Technology, Dept. of Electrical Engineering and Computer...
Very Low Frequency (VLF 3-30 kHz) receivers are used to monitor the amplitude and phase of signals f...
It is possible to observe and control to a limited extent the changes in characteristic ionospheric ...
The electron temperature changes due to 3, 5 and 430 MHz radio wave heating in the lower ionosphere ...