Magnetoplasma diffusion at F2 region altitudes
Magnetoplasma diffusion equation derivation for F-2 layer of ionosphere
F-2 LAYER↗
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The variability of ionospheric parameters
Seasonal variation of standard deviation of hourly values of F-2 layer
F-2 LAYER↗
The electron density distribution in the f sub 2-layer of the ionosphere in winter.
Wintertime f-2 layer electron density distribution, relating ionization increase to magnetic dip, solar cycle and winter anomaly
F- 2 LAYER↗
THE ELECTRON DENSITY DISTRIBUTION IN THE F SUB 2 LAYER OF THE IONOSPHERE IN WINTER
Electron density distribution in the f-2 layer of the ionosphere in winter, and the relation of the enhanced ionization to the so-called winters anomaly
F LAYER↗
Atmosphere of Mars - Mariner IV models compared.
Mariner IV models of three Mars atmospheric layers analogous to terrestrial E, F-1 and F-2 layers, considering relative mass densities, temperatures, carbon dioxide photodissociation and ionization profile
MARS ATMOSPHERE↗
Ionization transport effects in the equatorial F region.
Continuity equation for electrons in F-2 layer obtained for region near geomagnetic equator at noon including photoionization, recombination, drift, etc
F- 2 LAYER↗
The midlatitude ionospheric response to fluctuations in solar activity under low geomagnetic activity conditions
The ionospheric response, which is the sensitivity and delay of the electron content to the 270 day fluctuations of solar radiation has been theoretically analyzed. In the context of the present work the sensitivity is defined as the magnitude of the electron content fluctuation for a given change in solar flux, and the delay is defined as the timeshift of the response of the electron content to fluctuations in solar flux. Both the model in which the action of neutral winds on the F-2 layer is disregarded and that in which the wind effect is included as part of a positive feedback mechanism, are studied. It is shown that the neutral winds play a dominant role in the mentioned ionospheric response. The computed delays decrease with increasing solar activity in both models.
Bendito, J. L.↗
Variations in the altitudes of the maximum electron concentration of the f2 region <izmeneniye vysot maksimal'noy elektronnoy kontsentratsii oblasti f2<
Variations in altitudes of maximum electron concentration of f- 2 layer
ALTITUDE↗
THE ELECTRON DENSITY DISTRIBUTION ON THE F SUB 2 LAYER OF THE IONOSPHERE IN WINTER
Electron density distribution in ionosphere f2 layer in winter
F-2 LAYER↗
Spatial distribution of anomalous ionization in the f2 layer at high latitudes <prostrans- tvennoye raspredeleniye anomal'noy ionyzatsii v sloye f2 v vysokikh shirotakh<
Spatial distribution of anomalous ionization in f- 2 layer at high latitude
F-2 LAYER↗
Latitudinal and seasonal distribution of the daily maxima and minima of f0f2 values <o shirotnom i sezonnom raspredelenii maksimal'nykh - minimal'nykh sutochnykh znacheniy f0f2<
Latitudinal and seasonal distribution of daily maxima and minima of f- 2 layer critical frequencies
CRITICAL FREQUENCY↗
Influence of the earth's magnetic field on the diurnal variation of foF2 /Fourier analysis/
Fourier analysis of diurnal variations in F- 2 ionospheric layer induced by earth magnetic field
MAGNETIC FIELD↗
A topographical study of the f2 region of the ionosphere
Measuring ionospheric electron density in F- 2 layer - diurnal variation
IONOSPHERIC ELECTRON DENSITY↗
THE ELECTRON DENSITY DISTRIBUTION ABOVE THE F2 PEAK AND ASSOCIATED ATMOSPHERIC PARAMETERS
Atmosphere and electron density distribution above f2 peak
ELECTRON DENSITY↗
Dynamic diffusion processes in the exosphere.
Proton diffusion processes in exosphere, noting importance in determining ion scale height above f-2 peak
GREENHOUSE EFFECT↗
Effect of the Starfish high altitude nuclear explosion on the F2-region.
Star Fish high altitude nuclear explosion effect on electron loss rate in F-2 region
ELECTRON DENSITY PROFILE↗
Anomaly of the composition of the F-2 equatorial region of the ionosphere during the hours after sunset according to data from the mass-spectrometer experiment on the Cosmos-274
A mass spectrometer on board Cosmos-274 measured concentrations of light atoms and ions. While traversing the geomagnetic equator during the evening hours it recorded on anomalous drop in ionized molecular oxygen and ionized atomic oxygen and nitrogen. A similar, less dramatic, decline was observed in the concentration of neutral atomic oxygen. A possible explanation for this and previously observed behavior is an ascent in altitude of the F layer in the hours after sunset, a possibility which is supported by calculations.
Gaydukov, V. Y.↗