“…Generally the climate of this region arises from a complex interaction of synoptic scale regional and local controls (Ryan, 1992;Kounkou et al, 2009). On the synoptic scale the region is under the influence of mainly drier westerly airstreams in the winter and predominantly moist easterly air streams in the summer months (Linacre and Hobbs, 1977;Knight and Knight, 2001;BoM, 2012b). Each year, many thunderstorms occur in the region, some of which are strong enough to produce one or more of disastrous costly effects in the GMSTWA (Kuleshov et al, 2002;Davies et al, 2008).…”