A rapidly convergent procedure for computing large-scale condensation in a dynamical weather model
By: W. E. Langlois
Abstract
A generalized Newton-Raphson procedure is used to calculate the amount of moisture which should be removed when the air in a grid cell of a dynamical weather model becomes supersaturated. A test of the procedure shows that iteration is unnecessary: one pass leaves a residual supersaturation in the parts per million range.
DOI: https://doi.org/10.3402/tellusa.v25i1.9636 | Journal eISSN: 3035-9554
Language: English
Page range: 86 - 87
Submitted on: Aug 22, 1972
Published on: Jan 1, 1973
Published by: Stockholm University Press
In partnership with: Paradigm Publishing Services
© 1973 W. E. Langlois, published by Stockholm University Press
This work is licensed under the Creative Commons Attribution 4.0 License.