๐”– Bobbio Scriptorium
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On the use of a simple two-level model in general circulation studies: A note on the dependence of atmospheric predictability on baroclinic development

โœ Scribed by P. J. Everson; D. R. Davies


Publisher
John Wiley and Sons
Year
1972
Tongue
English
Weight
251 KB
Volume
98
Category
Article
ISSN
0035-9009

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๐Ÿ“œ SIMILAR VOLUMES


A note on the dependence of atmospheric
โœ P. J. Everson; D. R. Davies ๐Ÿ“‚ Article ๐Ÿ“… 1971 ๐Ÿ› John Wiley and Sons ๐ŸŒ English โš– 270 KB

## Abstract A twoโ€level, quasiโ€geostrophic model, described by Everson and Davies (1970), is used to study the dependence of duration of predictability (as defined by, e.g., Charney et al. 1966) on the phase, at some initial time in the integration, of global scale baroclinic development (expressed

On the use of a simple two-level model i
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## Abstract Numerical experiments with a twoโ€level, quasiโ€geostrophic model, described by Davies and Davies (1969), have been extended in several ways; the grid spacing of the previous model has been halved, greatly reducing numerical errors, and the lateral Eastโ€West span of the flow domain is muc

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## Abstract In a paper by Davies and Oakes (1962) concerning the problem of formulating a model of the general atmospheric circulation, the boundary condition used at the surface of the earth involved the assumption that the surface meridional, zonal, and vertical velocities are zero. In this note

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## Abstract Angular momentum transports due to mean meridional circulations and horizontal exchange processes are computed for a theoretical model. It is found that, in high latitudes, the transport due to mean meridional circulations is less than 1 per cent of that due to horizontal exchange proce

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Under the general Gauss-Markov model {y, XI~, a 2 V}, equality of MINQUE and so called 'simple' estimator (1/f)y v (I -XX+)y with f=rank(X:V)rank(X) for 0 "2 is considered. It is revealed that this equality holds if and only if the quadratic form (1/a2)yT(l --XX +)y admits a xZ-distribution under no