Abstract
A squall line of the southwest monsoon season has been analysed based on the radarscope observations and the prevalent synoptic situations, It was found to have a regenerative drift. It dissipated gradually after travelling some distance over land. The dimension of a single convective cloud cell inferred from a study of the associated changes in the meteorological elements observed at Dum Dum and Alipore appeared to be much in exceis of what has been found in the Thunderstorm Project.
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