Interaction of two baroclinic waves as a result of the daily variation of the stability of the atmosphere
Article
Received:
- 13 Downloads
Summary
A schematic theoretical explanation of one type of cyclogenesis, described in detail in [1], is presented. From a theoretical point of view, a “parameteric instability” of a system of two baroclinic waves (a synoptic trough and a sub-synoptic, locally conditioned wave), associated with the daily variation of the vertical stratification of the atmosphere, is involved. The theoretical possibility of explaining the interaction of the waves itself, based on the outflow of cold air from the region of the trough towards the sub-synoptic wave (the so-called jump of the cold front), is investigated.
Keywords
Atmosphere Stratification Structural Geology Theoretical Point Daily Variation
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.
Preview
Unable to display preview. Download preview PDF.
References
- [1]J. Štekl: Orographic Trough or Low in the Alpine Region (and Their Effect on Weather in the CSR). Travaux Inst. Géophys. Acad. Tchécosl. Sci., No. 535, Travaux Géophysiques 1979, Academia, Praha (at press).Google Scholar
- [2]J. Brádka: Přechody front Prahou. Meteor. zpr., 14 (1961), 58.Google Scholar
- [3]E. Čechová: Horizontální proměnlivost stabilitního parametru. ÚFA ČSAV, Praha 1975 (not published).Google Scholar
Copyright information
© ACADEMIA Publishing House of the Czechoslovak Academy of Sciences 1981