β Scribed by D. G. James
No coin nor oath required. For personal study only.
A description is given of one flight below cumulus clouds on 28 Aug. 1952. Small rapid fluctuations of temperature were observed by a sensitive resistance thermometer, records being obtained as a photographic trace. It is shown that, with respect to the frequency and type of fluctuation of temperature encountered, the space between cloud base, i.e., 3,100 ft, and ground level may be divided into three sections. The first, a layer extending from ground to about 800 ft, the second from 800 ft to about 2,800 ft, and the third from 2,800 ft to cloud base. A possible explanation for the formation of these layers is discussed.
π SIMILAR VOLUMES
## Abstract Cloud particles of diameters greater than about 100 ΞΌ can be sampled from an aircraft by exposing within the cloud a thin aluminiumβfoil surface to the airstream and counting and sizing the indentations made on it. A series of flights has been made through cumulus clouds using this tech
The fluctuation current through a Josephson junction has been calculated, one side of which is a stable superconductor, the other a fluctuating one. The theoretical functions cover the frequency range O-< to <3.5A. They reflect the characteristic experimental features in a consistent picture. In add