Positive ion composition and density in the lower E-region, from 87 to 114 kilometers
Positive ion composition and density in lower E region measured by mass spectrometry
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Positive ion composition and density in lower E region measured by mass spectrometry
Ionospheric E region irregularities produced by nonlinear coupling of unstable plasma waves
E-layer ionization and solar X-ray emission in 44-60 angstrom band
IMP-E flight plan, communications system, power supply, attitude control system, contamination monitor, experiments, and Delta launch vehicle
Integrated set of three detectors for galactic and solar ray studies of OGO-E and OGO-G
Electron density profiles of Nike-Apache rocket observations of nitric oxide ionization by Lyman alpha radiation in E region at sunrise
Diurnal variation of sporadic E at high latitude as function of geomagnetic activity
Geomagnetic field variations in temperate zone sporadic E layer according to wind-shear theory
Positive ion layers in E region explained by wind shear theory, obtaining steady state solutions for simple model
Electron and ion temperature changes in sporadic E layer based on wind shear theory, using energy equation
Lower E-region positive ion concentrations measured at time of declining solar activity by rocket installed mass spectrometer
Ionospheric E region dynamical processes, discussing energy phenomena of planetary waves, tidal oscillations and gravity waves
Electron temperature observation in E region with Langmuir probes on Nike Apache rockets, discussing solar radiation effect
Computer program for OGO-E vehicle response analysis to transient loading during Atlas booster burnout
OGO-E plasma spectrometers for measuring total flux below 12 kev and energy /spectral density/ of plasma
Analysis of wind and electron density profiles of E-region obtained from Nike-Apache rockets launched 22 Feb. 1968
Channel multiplier spectrometer for low energy electrons and protons at synchronous altitude on ATS-E satellite