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<br />METEOROLOGY. HYDROLOGY. BIG THOMPSON RIVER AND CACHE LA POUDRE RIVER BASINS 45 <br /> <br /> <br />20 <br /> <br />DISTANCE FROM STORM MOUNTAIN. IN MILES <br />10 0 10 <br /> <br />20 <br /> <br />18 <br /> <br />17 <br />18 __~.~.::::---,..;:.. <br /> <br />15 -~~---- <br />" <br /> <br />:1 14 <br />w <br />t; <br />:; 13 <br />~ <br />'" <br /> <br />'" <br />'" 12 <br />z <br />< <br />'" <br />::> <br />'" 11 <br />:c <br />.... <br />~ <br />...1 10 <br />~ <br />::5 9 <br />'" _250 C <br />z <br />::5 8 <br />:; <br />w <br />e; 7 <br />Ol <br />< <br />'" 6 <br />'" <br />::> <br />I:: <br />!:i 5 <br />< <br /> OoC <br /> 4 <br /> <br />30 <br /> <br />10 0 10 20 <br />DISTANCE FROM STORM MOUNTAIN, IN KILOMETERS <br /> <br />30 <br /> <br />20 <br /> <br />..: SCHEMAnC LINES OF AIRFLOW <br />I1111111111 SCHEMAnC AREA OF RAINFALL <br /> <br />EXPLANATION <br />-LFC- LEVEL OF FREE CONVECTION <br />-LCL- LIFTED CDNDENSAnDN lEVEL <br /> <br />-/5- RADAR REFLECTIONS OBSERVED AT GROVER, COLO, --DIShed <br />where epproximlltely located. IntervallD dBZ <br />- 0"- LINE OF EOUAl AIR TEMPERATURE, IN OEGREES CELSIUS.- <br />Dashed within the cloud <br /> <br />30 <br /> <br />60 <br /> <br />55 <br /> <br /> 50 <br />J' <br /> 45 <br />J t; <br /> ~ <br /> ~ <br /> '" <br /> 40 '" <br />\ '" <br /> z <br /> < <br /> '" <br /> ::> <br /> '" <br /> 35 :c <br /> .... <br />'\ ~ <br /> ...1 <br /> w <br /> 30 ~ <br />\ ::5 <br /> '" <br /> z <br /> 25 ::5 <br /> :; <br />J' '" <br /> e; <br /> III <br /> < <br /> 20 w <br /> '" <br /> ::> <br /> .... <br />J' 6 <br /> < <br /> 15 <br />LFC <br />~ 10 <br /> 5 <br /> <br />40 <br /> <br />J' <br /> <br />W1ND..QIRECTION AND SPEEO OBSERVATION.-Sheft Indi- <br />cates wind direction; north is at top. Barbs on shaft indicate <br />wind speed. in knots. Flag = 50 knots; long barb "" 10 knots; <br />short barb"" 5 knots <br /> <br />FIGURE 39.-Phyeical model of the thunderstorms over the Big Thompson River area at 1845 MDT, July 31. 1976. <br /> <br />/3- <br />