A study of mesoscale convective bands behind cold fronts. Part I: Mesoscale organization

Abstract This paper reports observations made over the North Atlantic of a system of convective cloud bands found within the cold air behind an occluded front. The observations were made from an instrumented aircraft which additionally released a pattern of dropsondes, measuring temperature, relativ...

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Bibliographic Details
Published in:Quarterly Journal of the Royal Meteorological Society
Main Authors: Bennetts, D. A., Ryder, P.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 1984
Subjects:
Online Access:http://dx.doi.org/10.1002/qj.49711046310
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fqj.49711046310
https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/qj.49711046310
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Summary:Abstract This paper reports observations made over the North Atlantic of a system of convective cloud bands found within the cold air behind an occluded front. The observations were made from an instrumented aircraft which additionally released a pattern of dropsondes, measuring temperature, relative humidity and wind, as functions of pressure. These data are analysed to establish some of the mesoscale, cloud‐scale and microphysical properties of the system. Here, in part I, the mesoscale structure is described and compared with the predictions of various theoretical models. The convective cloud structure emerges as a consequence of the mesoscale organization but appears to play only a minor role in its creation and maintenance. One of the theoretical models considered, conditional symmetric instability, provides a piausible explanation of the mesoscale observations.