Photoelectron heating efficiency in the ionosphere.
Photoelectron heating efficiency in ionosphere, using Thomson scatter data
Cohen, R.↗
Engineering topics
Hanson, W. B.
Publications and source records attributed to Hanson, W. B..
Planetary atmospheres
Planetary atmospheres data in 1967 for Venus, Mercury, Mars, Jupiter, Earth, and Moon
Colegrove, F. D.↗
Sodium distribution in the upper atmosphere.
Sodium distribution in upper atmosphere investigated in terms of photoionization lifetime, eddy diffusion and scale height
Donaldson, J. S.↗
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↗
Atmospheric composition in the lower thermosphere.
Atomic-to-molecular oxygen concentrations ratio values in upper atmosphere used to determine strength of turbulent mixing in atmosphere, noting definition of turbopause height
THERMOSPHERE↗
Comment on a paper by Thomas P. Quinn and John S. Nisbet, ''Recombination and transport in the nighttime F layer of the ionosphere.''
Ambipolar diffusion parameter calculation by Quinn and Nisbet found erroneous for night F layer
NIGHT IONOSPHERE↗
Eddy diffusion and oxygen transport in the lower thermosphere.
Eddy diffusion and oxygen transport in lower thermosphere
THERMOSPHERE↗
Effect of ionization transport on the equatorial f-region.
Ionization transport effect on equatorial F region, using numerical solution of steady state continuity equation
F LAYER↗
Investigations of the neutral composition of the upper atmosphere final report
Nike-Apache meteorological rocket for investigation of neutral composition of upper atmosphere
UPPER ATMOSPHERE↗
The maintenance of the night-time f-layer.
Nighttime F layer maintained by hydrogen ions providing source of oxygen ions through charge exchange or by upward drift of ionization
NIGHT IONOSPHERE↗
The maintenance of the nighttime f-layer
Nighttime F layer maintenance - protonosphere ion source and effective recombination coefficient
F LAYER↗
Dynamic diffusion processes in the exosphere.
Proton diffusion processes in exosphere, noting importance in determining ion scale height above f-2 peak
GREENHOUSE EFFECT↗
DIURNAL VARIATION OF THE HYDROGEN CONCENTRATION IN THE EXOSPHERE
Lateral flow and other effects contributing to the diurnal variation of the amount of atomic hydrogen in the exosphere
DIURNAL VARIATION↗
THE DISTRIBUTION OF INTERPLANETARY HYDROGEN
Calculation of atomic hydrogen distribution in interplanetary space based on solar wind measurements
SOLAR WIND↗
THE DISTRIBUTION OF INTERPLANETARY HYDROGEN
Solar wind distribution of neutral interplanetary hydrogen by interaction with solar protons
INTERPLANETARY GAS↗
Diurnal Variation of the Hydrogen Concentration in the Exosphere
Diurnal variation of hydrogen concentration in exosphere
DIURNAL VARIATION↗
ELECTRON TEMPERATURES IN THE UPPER ATMOSPHERE
Energy loss processes for fast electrons, electron heating efficiency, heat input to the electron gas, effect of thermal coupling, and electron thermal conductivity above the f2 peak
F- 2 LAYER↗