Abstract: No abstract available.

Abstract: It is shown that the vertical motion due to flow over irregular terrain may be calculated from a simple formula in an atmosphere whose static stability is a function of pressure only. Some computations are presented to ...

Abstract: A boundary layer model, to investigate various aspects of desert circulation, has been devised. The planetary boundary layer is divided into a surface (constant flux) layer, a transition layer and an inversion layer. The ...

Abstract: No Abstract Available

Abstract: tract

Abstract: tract

Abstract: tract

Abstract: From the premise that the modelling approximation for an integrated numerical-prediction model is given by a constraint on the stability factor in the first law of thermodynamics for adiabatic flow, a three-parameter ...