Exobase hydrogen density temperature from Lyman alpha absorption and polarization measurements. II - Dayside and nightside results during April 1971

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Geocoronal Emissions, Hydrogen, Lyman Alpha Radiation, Molecular Absorption, Polarimetry, Polarized Electromagnetic Radiation, D-2 Satellites, Data Processing, Daytime, Diurnal Variations, Gas Density, Night Sky, Oxygen Spectra

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The measurements of polarization and absorption of the Lyman alpha geocoronal emission discussed in this paper were carried out on board the French spacecraft D2-A Tournesol during the period from April 19 to May 2, 1971. The measurements are compared with theoretical predictions from spherical models of transfer constructed using a Knockerts-Nicolet distribution of hydrogen from 100 to 500 km and a Chamberlain distribution from 500 to 100,000 km. A hydrogen density of (10 plus or minus 2) x 10,000 atoms per cu cm at noontime near the equator was deduced from the polarization measurements. The respective midnight density was (11 plus or minus 3) x 10,000 atoms per cu cm. The midnight to midday density ratio was roughly 1.1. The intensity of the extrageocoronal Lyman alpha background, measured in a plane perpendicular to the sun-earth axis varied between 780 and 430 R.

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