Answers are grounded in this paper and cite their sources.
Electron densities in the ionosphere above White Sands, New Mexico, were measured continuously from the E region up to the lower F2 region with the Aerobee-Hi NRL No. 50, a rocket instrumented by the U.S. Naval Research Laboratory. This rocket was fired at 12:09 p.m. MST on 29 June 1956 and reached an altitude of 263.7 km. The method1 used consists in refractive index measurements based on propagation phenomena. Two harmonically related c-w signals, at 7.75 Mc and 46.5 Mc, respectively, are transmitted from the moving rocket to two receiving stations on the ground. The rocket motion causes each signal to experience a Doppler shift, which is related to the refractive index of the medium near the rocket. The high frequency is used as a reference, since its index is essentially unity. Comparison techniques used on the ground plus a knowledge of the rocket trajectory yield, as a function of altitude, the 7.75-Mc refractive indices for both ordinary and extraordinary rays. Since the electron density can be computed from either index, a check of the internal consistency of the data is possible.
No takes yet. Share an insight, caveat, or question.
Jackson et al. (1956) studied this question.
Synapse has enriched 10 related papers. Consider them for comparative context: