Abstract
It is well known that in higher latitudes the lower parts of cumulonimbus may precipitate completely leaving only the anvil. It is also well known (KOTSCH, 1947) that in tropical latitudes precipitation occurs from clouds which have not reached the freezing level. Finally, it is known, at least to most tropical meteorologists, that quite commonly in the tropics a cumulus cloud will precipitate completely.
DOI: https://doi.org/10.3402/tellusa.v3i3.8627 | Journal eISSN: 3035-9554
Language: English
Page range: 203 - 204
Published on: Jan 1, 1951
Published by: Stockholm University Press
In partnership with: Paradigm Publishing Services
© 1951 L. Sherman, published by Stockholm University Press
This work is licensed under the Creative Commons Attribution 4.0 License.
