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<br />28. Locations of lightning strikes for Owl Creek Pass ewnt of August 21,1995 51 <br />29. Skew-T diagram showing the Albuquerque evening sounding for August 21, 1995 (0000 UTC on <br />August 22). Occurrence elevation! process curve, precipitable water adjusted to occurrence elevation, <br />stability data, and QPF indicated. 53 <br />30. Same as Figure 29 but for Grand Junction. 54 <br />31. NLDN Lightning Report for Pagosa Springs, Colorado event. 55 <br />32. Reconstructed composite of storm locations based on cloud-tn.-ground lightning strokes during the <br />Pagosa Springs event. Strike location indicated by a dot. 56 <br />33. Storm 3 positions based on lightning stroke locations from 1825 to 1905l\1DT OIl August Z2~ 1995 Strike <br />locations indicated by a dot. 57 <br />34. Storm 3 positions based on lightning stroke locations from 1905 to 1925 MDT on August 22, 1995. Strike <br />locations indicated by a dot. 58 <br />3S. Storm 3 positions based on lightning stroke locations from Ins to 19S0 MDT on August 22, 1995. Strike <br />locations indicated by a dot. 59 <br />36. Skew-T diagram showing the Albuquerque eveuiug sounding for August 22, 1995 (OOOIJUTC on <br />August 23). Occurrence elevation, process curve, precipitable 'Y~lter adjusted to occurrence elevations, <br />stability data, and QPF indicated.' . 61 <br />37. Same as Figure 36 but for Grand Junction. 62 <br />38. :tHap showing three thunderstorm formation areas active during the Pagosa Springs event of <br />August 22, 1995. Low-level inflow fetch also indicated., 63 <br /> <br />LIST OF TABLES <br /> <br />TABLE <br /> <br />PAGE <br /> <br />I. A sample of raw lightning data used for plotting IS-minute CG charts. Columns are date and <br />time (UTe), latitude and longitude of each stroke in degrees and fractions of a degree, stroke strength <br />in kiloamperes, and stroke distance and bearing from center reference point. 30 <br />2. Areal coverage (sq. mi.) and IS-minute CG production by the Opal Storm Cells between <br />41S PM (LDT) and 600 PM (LDl'). 41 <br />3. Summary of meteorological components associated ,Yi1:ll Hash flooding. 66 <br />4. Comparison of meteorological cbaracteristics of llash llooding events east and west of the <br />Continental Divide at elevations above 6000 feet msI.. 67 <br /> <br />IV <br />