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Horizontal diffusion in the atmosphere: A lagrangian dynamical theory

✍ Scribed by F.B. Smith


Book ID
113121726
Publisher
Elsevier Science
Year
1983
Tongue
English
Weight
531 KB
Volume
17
Category
Article
ISSN
0004-6981

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πŸ“œ SIMILAR VOLUMES


Theory of non-horizontal adiabatic flow
✍ R. S. Scorer πŸ“‚ Article πŸ“… 1955 πŸ› John Wiley and Sons 🌐 English βš– 555 KB

## Abstract The equation of continuity takes the form when there are appreciable vertical displacements (see Section 1 for list of symbols). The stream function, Ξ¦, for two‐dimensional steady motion satisfies an equation which for vertical displacements of less than about a kilometre reduces to t