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Baroclinic instability in the summer mesosphere

✍ Scribed by A. J. Simmons


Publisher
John Wiley and Sons
Year
1977
Tongue
English
Weight
316 KB
Volume
103
Category
Article
ISSN
0035-9009

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✦ Synopsis


Abstract

Baroclinic instability is examined in idealized models of the summer circulation of the upper stratosphere and mesosphere. For all but possibly the fastest rate of thermal dissipation, results suggest the development of disturbances which have zonal wavelengths around 5000 km and which move with westerly phase speeds between 5 and 10 m^βˆ’1^ relative to an easterly maximum. Their periods relative to the ground are close to one day. the vertical scale of perturbation velocities is some 15 km. Temperatures exhibit a shorter vertical scale of about 5 km or less.


πŸ“œ SIMILAR VOLUMES


Primary and secondary bifurcation in bar
✍ A. Lorenzen; G. E. A. Meier; M. Assenheimer; E. -A. MΓΌller πŸ“‚ Article πŸ“… 1990 πŸ› Springer 🌐 English βš– 879 KB

In modelling atmospheric flows the baroclinic instability of the flow in a differentially heated rotating annulus plays a central role. This paper deals with an experimental study using LDV and flow visualization techniques. Usually the temperature difference, AT, was kept fixed while the angular ve