## Abstract Three kinds of flow over unlevel ground are defined according to their scale โ aerodynamic, barostromatic, and geostrophic flow โ and it is seen that the practical difficulties in the way of obtaining the correct value of the relevant nonโdimensional numbers in model experiments are alm
Theory of airflow over mountains: III - Airstream characteristics
โ Scribed by R. S. Scorer
- Publisher
- John Wiley and Sons
- Year
- 1954
- Tongue
- English
- Weight
- 758 KB
- Volume
- 80
- Category
- Article
- ISSN
- 0035-9009
No coin nor oath required. For personal study only.
โฆ Synopsis
Abstract
The problem of what second boundary condition (the first being the ground profile) should be applied to the differential equation for the variation with height of the wave amplitude is considered and it is thought that solutions corresponding to upward and downward progressing waves are generally irrelevant. In practice we shall be concerned mainly with those waves of length such that their amplitude decreases with increasing height. Only when there is a considerable range of such wavelenghts is the motion of the kind supposed in the perturation theory.
Though it is desirable to characterize an airstream by a single number this is not at present possible for airstreams in general, and it is shown by examples how airstreams may possess the same lee wave length though their lโprofiles differ considerably. These examples show that generally the maximum amplitude of the waves is found at or close to levels of maximum values of l, at sharp inversions in particular.
The behaviour of lee (statopmaru) waves is fairly representative of mountain waves in general.
๐ SIMILAR VOLUMES
## Abstract Separation of flow may be twoโdimensional when the wake or eddy is closed, or threeโdimensional when the air is continuously replaced. It often occurs at a salient edge. When it occurs the effect of the mountain on the highโlevel flow is reduced. If the airflow is temporarily induced to