Abstract
An earlier theory of steady state, saturated convective currents is modified to include the drag of the condensed liquid water on the rising air. The system of equations is numerically integrated for several cases in which the entrainment is allowed to assume negative values. Results appear to indicate improvement over the earlier model.
DOI: https://doi.org/10.3402/tellusa.v12i4.9417 | Journal eISSN: 3035-9554
Language: English
Page range: 393 - 398
Published on: Jan 1, 1960
Published by: Stockholm University Press
In partnership with: Paradigm Publishing Services
© 1960 G. J. Haltiner, E. M. Chase, published by Stockholm University Press
This work is licensed under the Creative Commons Attribution 4.0 License.