Radar composite images of the German Weather Service's (DWD) radar network are used to investigate the spatial and temporal structure of convective rain areas in postfrontal situations. Thirty-nine days were selected and the respective postfrontal convective rain fields were analysed based on over 3000 radar images, yielding altogether approximately 140000 individual rain areas. Basic parameters of the latter within the convective area such as number of rain areas, occupied area and number of reflectivity peaks contained within one single rain area were determined. Then their diurnal variation and spatial distribution within Germany were investigated. The study focuses on single cells (rain areas with one reflectivity peak) and clusters (rain areas with two or more reflectivity peaks), with the latter being defined as consisting of several interconnected convection cells. Number and area of rain areas follow the expected, typical convective diurnal cycle with a maximum around noon. The number ratio of single cells and clusters, however, remains almost constant over the day. This surprising result may be explained as an equilibrium state between growing single cells, the development of single cells into clusters and decaying of single cells and clusters. Similar results are found for the area covered by single cells or clusters. While single cells dominate in terms of number, clusters provide most of the precipitating area. Single convective cells and small clusters preferably occur over mountain ranges but also along the North Sea coast. Large clusters with more than 9 reflectivity maxima are almost exclusively found along the North Sea coast in an area of about 200 km width.
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