Newton et al. 1964
Newton, G., R. Horowitz, and W. Priester, 1964: Atmospheric densities from Explorer 17 density gages and a comparison with satellite drag data. J. Geophys. Res., 69, 4690-4692.
The purpose of this letter is to present the initial atmospheric densities directly measured by the ionization gages on the Explorer 17 satellite. The satellite has been described [Horowitz, 1963] and the gages and their response to the atmosphere have also been reported [Newton et ai., 1963]. The data presented in this letter were obtained with two types of ionization vacuum gages, the hot-filament thermionic type (Bayard-Alpert) and the magnetron type (Redhead). The absolute accuracy of these data is believed to be °35% and the repeatability is °20%. A more complete discussion of the experiment will be included in a paper now in preparation [Newton et ai., 1964].
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Newton, G., Horowitz, R., and Priester, W.: Atmospheric densities from Explorer 17 density gages and a comparison with satellite drag data, J. Geophys. Res., 69, 4690-4692, 1964.
Newton, G., R. Horowitz, and W. Priester (1964), Atmospheric densities from Explorer 17 density gages and a comparison with satellite drag data, J. Geophys. Res., 69, 4690-4692.
Newton, G., R. Horowitz, and W. Priester, 1964: Atmospheric densities from Explorer 17 density gages and a comparison with satellite drag data. J. Geophys. Res., 69, 4690-4692.
Newton, G., Horowitz, R., & Priester, W. 1964, J. Geophys. Res., 69, 4690.
Newton G, Horowitz R, Priester W. Atmospheric densities from Explorer 17 density gages and a comparison with satellite drag data, J Geophys Res 1964;69:4690-4692.
G. Newton, R. Horowitz, W. Priester, J. Geophys. Res. 69, 4690-4692 (1964).