Abstract
Empirical results indicating similar turbulent transfer for cloud droplets and for water vapour or sensible heat have been used in order to derive a set of prognostic equations for the total moisture content and for the equivalent potential temperature. With given external conditions, especially imposed vertical velocity the equations can be used for forecasting the formation and development of layer clouds. An example of practical application is discussed.
DOI: https://doi.org/10.3402/tellusa.v16i2.8926 | Journal eISSN: 3035-9554
Language: English
Page range: 139 - 146
Submitted on: Jun 13, 1962
Accepted on: Jun 15, 1963
Published on: Jan 1, 1964
Published by: Stockholm University Press
In partnership with: Paradigm Publishing Services
© 1964 L. T. Matvejev, published by Stockholm University Press
This work is licensed under the Creative Commons Attribution 4.0 License.
