“…The spatial and temporal characteristics of convective activity have been observed, and in some cases predicted, from conventional climatology, the application of statistical models, and the use of remotesensing techniques. Remote sensing by weather radar was used to define convective climatologies for specific locations by Frank et al (1967), Scott (1967), Owens (1969), Muench (1976), and Falconer (1984). A convective 0899-841 8/89/06058 1-20$10.00 0 1989 by the Royal Meteorological Society climatology derived from radar observations permits the desired spatial and temporal resolution unavailable in the absence of a high-density observation network.…”