Abstract
It is proposed that certain characteristic stratifications accompany cumulus and cumulonimbus, and on the basis of a thermal theory characteristic magnitudes are estimated for the properties of their updraughts, and the size which must be attained by cumulus before showers form and their transformation into cumulonimbus occurs.
DOI: https://doi.org/10.3402/tellusa.v18i4.9689 | Journal eISSN: 3035-9554
Language: English
Page range: 687 - 698
Submitted on: Jan 10, 1966
Published on: Jan 1, 1966
Published by: Stockholm University Press
In partnership with: Paradigm Publishing Services
© 1966 F. H. Ludlam, published by Stockholm University Press
This work is licensed under the Creative Commons Attribution 4.0 License.
