On cumulus mergers

Joining together or merging is postulated to be a major way in which convective clouds become larger, enhancing their transports and impacts upon their environment. Cumulus shower merger is defined in terms of echoes from a calibrated digitized 10-cm radar reviewing a 0.9×10⁵ km² area in south Florida, U. S. A., which encompasses a 1.3×10⁴ km² experimental area for randomized seeding. A detailed physical and statistical study is reported for three relatively undisturbed untreated days in the summer of 1973, the driest of which was a randomly selected control day for the experiment. Mergers are found to produce more than an order of magnitude more rain than unmerged echoes, while mergers of mergers (second order mergers) produce still an order of magnitude more rain. On the three days studied, merged systems produced about 86% of the rainfall over the area. Duration, echo area and rain depths are also compared for merged and unmerged systems. Each day is then analyzed individually, indicating a correlation between organization and rain amount, confirmed by other research reviewed briefly. The location and time of merger is related to the seabreeze convergence zones as predicted by the University of Virginia Mesoscale Model with overall good agreement. Physical hypotheses suggesting the importance of downdrafts in cumulus merging are developed. The relevance of mergers to hydrology, weather modification and the large-scale impacts of convective clouds is discussed.