D. Konovalov
The City College of the City University of New York
Keywords:
Meteorology, Atmospheric physics, Training
Abstract
We shall regard thermals as certain volumes of air at a temperature higher than that of the surrounding air which are rising from the Earth's surface and, during their vertical motion, are partially mixed with the ambient air having a lower temperature... In conclusion,..it is hoped that the data presented in this paper will prove useful for practical gliding objectives.
Author Biography
D. Konovalov, The City College of the City University of New York
