A scheme for the representation of the vertical eddy fluxes of heat, momentum and water vapour in a forecast model is presented. An important feature of the scheme is the dependence of the diffusion coefficients on the static stability of the atmosphere. Two tests are presented, using the scheme in
A model for proton interaction in the atmosphere including fluxes of generated electrons
β Scribed by H. Karszenbaum; D.A. Gagliardini
- Book ID
- 107935783
- Publisher
- Elsevier Science
- Year
- 1981
- Tongue
- English
- Weight
- 265 KB
- Volume
- 1
- Category
- Article
- ISSN
- 0273-1177
No coin nor oath required. For personal study only.
π SIMILAR VOLUMES
Previous work (Shuttleworth, 1976) demonstrated that 'multi-layer' simulation models of the vegetation-atmosphere interaction can be written in analytically continuous form: subsequent work (Shuttleworth, 1978) exploited the analytic nature of the model to simplify the description to a combination e
In this article we present a new method of Rossby asymptotics for the equations of the atmosphere similar to the geostrophic asymptotics. We depart from the classical geostrophics (see J. G. Charney [5] and our previous article [29]) by considering an asymptotics valid for the whole atmosphere, not