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Variable frequency VLF signals in the magnetosphere Associated phenomena and plasma diagnostics

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Variance of the phase fluctuation of a radio signal in the case of the normal sounding of the ionosphere

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Variation in the E layer during geomagnetic disturbances

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Variation of electron density along magnetospheric field lines as determined from POLAR spacecraft plasma wave observations

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Variation of fast charged particles in event of 22 November 1977 based on Cosmos-900 satellite data

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Variation of low-order acoustic solar oscillations over the solar cycle

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Variation of the flux of corpuscular radiation in the mid-latitude mesosphere by day

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Variation of the Martian Ionosphere from Mars Express Ionospheric Sounding

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Variation of the range-frequency characteristics of oblique sounding during the artificial disturbance of the upper ionosphere

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Variational inversion of the ocean acoustic tomography data using quadratic approximation to travel times

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Variations in concentrations of N/+/ and O/+/ ions, the dynamics of the ionosphere, and fluxes of energetic electrons in the earth's outer ionosphere on the meteor satellite. III - High-latitude ionosphere

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Variations in electron density in the middle latitude D-region above Urbana, Illinois

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Variations in flux of soft corpuscular radiation in the mesosphere at midlatitudes

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Variations in the altitude of the 5577 A emission layer

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Variations in the concentrations of O/+/ and N/+/ ions, the dynamics of the ionosphere, and fluxes of energetic electrons in the earth's outer ionosphere on the meteor earth satellite. I - Measurements in the mid-latitude ionosphere

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Variations in the height of an emission layer at 5577 A

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Variations in the ionospheric scale height parameter at the F2 peak over Grahamstown, South Africa

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Variations in the parameters of thunderstorm electromagnetic signals on paths over earthquake regions

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Variations of electron density in the D-region

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Variations of fast charged particles in the event of November 22, 1977 according to data of the Cosmos-900 satellite

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