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Rayleigh scattering intensities in the altitude range of 80-300 km are calculated using the concentrations of the principal atmospheric constituents N2, O2 and O. The polarizability of the oxygen atom is calculated from atomic oscillator strengths and normal and slant optical thicknesses are calculated as a function of altitude. (Author).
Investigates AF procedures and operations involved in an award of contract by the Electronic System Division, Hanscom Field, to TYCO Laboratories, Waltham, Mass.
Atmospheric density was determined from a singly mounted ionization gauge flown on an Air Force satellite. Included is a brief description of the experiment and theory as well as a discussion of some of the problems involved in performing these measurements. Density data are given for the altitude range of 370 to 400 km during early morning hours for the two days 17 and 18 June 1961. Results are compared with those of the 1961 revised U.S. Standard Atmosphere. (Author).
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Oceanographic engineer recounts his expeditions to find the fabled land called- The lost continent.