Variable eddy diffusivities and atmospheric cellular convection
โ Scribed by Durga Ray
- Publisher
- Springer
- Year
- 1986
- Tongue
- English
- Weight
- 729 KB
- Volume
- 36
- Category
- Article
- ISSN
- 0006-8314
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โฆ Synopsis
Using variable atmospheric eddy diffusivities, it is possible to obtain a theoretical explanation of observations concerning the increase of cell flatness in cellular cloud patterns. The inclusion of a horizontal variation of eddy size as proposed by and supported by Agee (1973) has a large intluence on theoretical Rayleigh number and cell shape, the degree of cell flatness being principally controlled by the degree of horizontal variation of the eddies. It is also shown that observations regarding the reversal of the circulation pattern could be interpreted on the basis of eddy diffusivities that change sign along the reference directions. This suggests that it may be useful to rethink our ideas about the existence of spatial variations in the eddy transfer coefficients in atmospheric convection.
๐ SIMILAR VOLUMES
An analysis of the stability and oscillation properties of upwind finite element methods for convectiondiffusion is given and used to develop a variable upwinding formulation. This formulation is particularly well suited to problems with nonconstant coefficients, nonlinearity or non-uniform meshes.
## Abstract Information on eddy diffusion in the atmosphere at heights between one and two kilometres has been obtained from an analysis of observations made on pairs of smoke puffs by using a camera obscura. The results are compared with a prediction of the Kolmogoroff similarity hypotheses.
## Abstract Methods of calculating the eddy diffusivity ฮบ are discussed. It is shown that methods which assume that ฮบ can be regarded as independent of the height, even through a shallow layer, lead to erroneous results: in consequence the frequent use in the literature of the approximate equation