The significance of dynamic instability in atmospheric motions
β Scribed by J. S. Sawyer
- Publisher
- John Wiley and Sons
- Year
- 1949
- Tongue
- English
- Weight
- 630 KB
- Volume
- 75
- Category
- Article
- ISSN
- 0035-9009
No coin nor oath required. For personal study only.
β¦ Synopsis
Abstract
A discussion is given of the criterion for a special type of dynamic instability first derived by H. Solberg, viz. :βthat the antiβcyclonic wind shear along an isentropic surface should exceed the coriolis parameter. It is concluded that this criterion has no direct bearing on the formation of extratropical cyclones but it may be important in respect of the limit which it imposes on the wind shear to the south of the βjet streamβ. Dynamic instability of this type may also be important in connection with the formation of tropical cyclones and certain features of frontal structure.
π SIMILAR VOLUMES
## Abstract A procedure is suggested by which an estimate of the ascent or descent of air can be obtained by use of constantβlevel maps and upper air soundings plotted on tephigrams or charts of a similar type. Results obtained by this method are compared with those by other methods. Examples of it
## Abstract The object of this paper is to show, in an elementary way, the general significance of the Richardson number for motions of a frictionless perfect gas of variable density subject to gravity. Dimensionless parameters like the Richardson number are important in relation to the concept of