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<br />28 <br /> <br />FLOOD, JULY 31-AUGUST 1, 1976, BIG THOMPSON RIVER, COLORADO <br /> <br /> <br />FIGURE 23.-Geostationary Operational Environmental Satellite photograph, 1600 MDT, July 31, 1976. Bright areas are clouds. <br /> <br />was 0.55 inch, substantially lower than 12 hours <br />earlier. However, precipitable water in the layer from <br />the surface to the 500-millibar level was 0.97 inch, <br />nearly the same as the morning value. Heating and <br />mixing had redistributed the moisture through a <br />thicker layer. The trailing front moved through <br />Denver, Colo., 15-20 minutes after the rawinsonde was <br />released. Therefore, the rawinsonde provided no infor- <br />mation about the extremely moist airmass just a few <br />miles to the northeast. <br /> <br />CONDITIONS DURING THE STORM <br /> <br />Prior to 1800 MDT, there had been almost no <br />precipitation falling on the foothills in northeastern <br />Colorado. Two to three hours later, catastrophic <br />flooding was occurring. This section describes <br />meteorological conditions along the Front Range from <br />Denver, Colo., to north of Fort Collins, Colo., from <br />1700 MDT to about 2200 MDT on July 31,1976. <br /> <br />Data were available from the following locations: <br />Fort Collins, Colo. (Colorado State University, At- <br />mospheric Science Building); Greeley, Colo. (Universi- <br />ty of Northern Colorado, Ross Hall); Table Mountain <br />near Boulder, Colo. (National Oceanic and At- <br />mospheric Administration, Environmental Research <br />Laboratories); Rocky Flats plant near Boulder, Colo. <br />(Rockwell International Corp.l; Jefferson County and <br />Arapahoe County Airports, Colo. (Federal Aviation <br />Administrationl; and Stapleton International Airport <br />in Denver, Colo. (National Oceanic and Atmospheric <br />Administration, National Weather Service). Radar <br />reflectivity data were available for the entire storm <br />from the radar operated by the National Weather Ser- <br />vice at Limon, Colo., located about 125 miles southeast <br />of the Big Thompson River area. Reflectivity data for <br />45 minutes at the beginning of the storm were <br />available from the radar used for the National Hail <br />Research Experiment at Grover, Colo., located about <br />70 miles east-northeast of the Drake-Estes Park area. <br />