Diagnosis and prediction of middle level cloud development associated with cold fronts over southern Australia
Autor: | S. E. Oliver, R. G. Tapp |
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Rok vydání: | 1989 |
Předmět: | |
Zdroj: | Meteorology and Atmospheric Physics. 41:231-246 |
ISSN: | 1436-5065 0177-7971 |
Popis: | Broad scale vertical velocities have been used to predict the development over southern Australia of cloud associated with cold fronts. The vertical velocities were determined by solving explicity the quasi-geostrophic omega equation expressed in terms ofQ-vectors. The frontal cloud band was located within the are where up-motion was diagnosed, with the deepest cloud in the vicinity of the strongest upward velocities, and the rear of the band coinciding closely with the change from up- to down-motion. On those occasions when a major cloud mass evolved the region of up-motion extended to low latitudes as a clearly defined band. This band was indicative free a well developed warm conveyor belt associated with the frontal system. Areas of diagnosed down-motion were free of deep, organised cloud masses. Stronger upward motion did not produce an immediate increase in the cloudiness; typically there was a delay of 12 to 24 h before the corresponding cloud development became apparent. |
Databáze: | OpenAIRE |
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