June 3, 2002 Eastern Colorado Hailstorm
Moist upslope flow and climatology sent us packing to eastern Colorado this day. As amazing as it might sound, there are hotspots east of the Rocky Mountain chain that are highly reliable severe thunderstorm generators. Under a given pattern of low-level winds and the presence of low-level moisture, one can often correctly choose on any given day which of the numerous topographic ridges in east-central Colorado will produce the best storm. This day it was fairly clear that the Palmer Divide southwest of Limon would be a good starting point. We headed to Limon and were soon greeted by a rather high-based, outflow dominant supercell storm that had little or no hope of producing a tornado. The reason for this mode of supercell was the lack of deep low-level moisture. As we drove towards Limon our onboard hygrometer measured dewpoints falling into the 40's. Had mid-50 dewpoints been present at the base of a deep, poorly-mixed moist layer the strong deep-layer shear probably would have supported tornadic storms.