Abstract
A balloon, the second In a series of high-altitude balloon flights, was launched to a record altitude of 50 km from White Sands Missile Range, N.M., on 22 September 1969. The 8.7 × 105 cubic meter, helium-filled, zero-pressure, polyethelene balloon served as a constant-level stable support for an instrument payload consisting of bead thermistor atmospheric and balloon-skin temperature sensors, thermal conductivity pressure gage, a forward-scattering beta-ray atmospheric density gage, chemiluminescent ozonesondes, a Geiger tube cosmic ray detector, and an accelerometer for the determination of the vertical component of balloon acceleration. Radar position-time data served to determine the wind velocity. Seven hours and 40 minutes of data were obtained from the various instruments at a near-constant altitude of 49 km (± 1 km). This paper discusses specifically the variations in the observed balloon trajectory, the supporting rocketsonde-determined winds, and the balloon-borne temperature sensor values as related to the existence of a diurnal atmospheric tide near 50 km. It also presents the related data obtained from the other instruments comprising the payload.
