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OPERATIONS: Low level moisture was carried into the region by easterly winds behind the cold front laying south of us. Late evening and morning drizzle, fog and low clouds covered most of the region periodically through Tuesday, By Tuesday afternoon the front moved northward over us as a warm front and began a trend of progressively hotter afternoon temperatures. Three periods of operations were conducted early in the week prior to afternoon heating becoming extreme in the last half of the week. One <operation was for rain stimulation, another for combined operations of rain augmentation and hail suppression and the last was purely for hail suppression, The warming trend which began Tuesday quickly brought record high surface temperatures to the region and much drier low levels ,in the atmosphere. Al J., times, liilted "below;,are ,in eDT. MAY 13th - OPERATIONAL DAY #7: Before sunup a clupter of severe storms deyeloped in southern Hamilton County. Only the cloud top aircraft was scrambled; low cloud ceilings and poor visibilities inhibited the safety of cloud base operations. In fact, due to the poor weather at the time in Dodge City, where the cloud top plane is based, the accuracy of the short-term forecast for improved weather conditions within the next two hours was critical to the aircraft launching. However, prior to take-off the aircraft' s tachometer cable broke requiring added time to repair it. Radar indicated hail in storms passing through southern Kearny County and was likely to have been present in other storms in parts of the counties: Hamilton, Stanton, Stevens, Grant and, perhaps, Haskell. By the time the aircraft launched and reached seeding altitude, the severe storms had decreased in iritensity and moved further east into the target area. Brief J;:ainfall stimulation seeding was attempted in Gray County' at 9 a.m., but conditions weren' t sui table for continued operations ,thereafter. MAY 14th - OPERATIONAL DAY #8: In early afternoon intense h~ating a 101"1 9' a section of the "dryline" began triggering new storm growth in extreme Southwest Kansas near Richfield. At 1:35 p.m. cloud base planes and the cloud top plane began being scrambled. Storms were expected to grow to become severe (hail-bearing). Seeding was initially performed to increase rainfall in weaker cloud updrafts found at 2:10 p.m. A second plane joined at 2:12 p.m. and began seeding the same storm. Cloud bases were high, near 14,OOD feet, and easterly storm movements carried the storm into northwestern Stevens County. The updrafts found at cloud base continued to be weak. However, at 2:23 p.m. radar showed its first indications of hail in the storm and hail suppression was begun. By 2:56 p.m. the storm had moved well into Stevens County and was exhibiting decreased intensity. Rain stimulation continued. Once again the storm pulsed indicating hail on radar such that at 3:18 p.m. hail suppression again was performed. The storm had moved into northeastern Stevens County by 3:36 p,m. and began dissipating. Two