Abstract
A scheme for parameterizing the effects of cumulus convection for the maintenance of the thermodynamic structure of the tropical atmosphere is described. This parameterization is used in a one-dimensional model that represents the vertical structure of the atmosphere as a function of Chebyshev polynomials. -from Author
Original language | English (US) |
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Pages (from-to) | 2166-2182 |
Number of pages | 17 |
Journal | Journal of the Atmospheric Sciences |
Volume | 40 |
Issue number | 9 |
DOIs | |
State | Published - 1983 |
ASJC Scopus subject areas
- Atmospheric Science