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<br /> <br />, <br />, <br />75(0' <br />, <br />~/ <br />lO~OO";" Austic"/ I <br />\',U } "-- <br />/-."",~/ <br />\ ,~" <br />\ ~~/ ~ ~ <br />-..,-".0/ ~---)GI! <br />~/ , Ha n <br />",f.;,:::;/ ,'",/ <br />:;.'->/ r) EltlS <br />,/ ~~~n!d ',_-..,park <br />. /. <br />,MaekJ <br />,Pn <br />1 <br />\We <br />I' <br />, <br />Nedurland <br />( , <br />" <br />/_) ';~1 <br />/'.Em <br />C____: <br /> <br />G~ende..v <br /> <br />.............:....6000:----- --'" <br />,r''" ,/ <br />/ , <br /> <br /> <br />5090' <br />\ /-----------~----- <br />~Ollins <br />. .. 'Windsor <br />, <br />tLoveland <br />\ <br />rthoud <br />0) <br />, <br />able f <br />. \ <br /> <br />).ele~ <br /> <br />G:anby <br /> <br />--~,,_//-"~,---.......... G' <br /> <br /> <br />~~;:,,,,", '.,~ <br /> <br />efMnverplJo <br /> <br />Eng!~ G~ <br />Airport /..---...... flJ!i!I" <br />. \ /--.rker "\, <br />Pin....--J ~,S al.. \ <br />.. ,'~ Castle, \ <br />, (.'.... /"'\" .Rack EI~labelh.c8;\ <br />'......... .. I \ - -" KIowa \ <br />') , .kefs " "... 6000' <br />'- /.' /' \ :'k'PU:......-____.Elbert <br />30 '-''-...} f // \ -', <br />" 7000. C <br /> <br />10000' <br /> <br />10 2'0 <br />km <br /> <br />750\ ..../::6000:--------) <br />',<lito ...... /' <br />G!endevey \, .,/ / <br />~.... <br />10000' /I <br />\ ,,..: RUll.ic/,' 5000' <br />I"~ U ..- \ <br />/-",,,,'t/ ... _---- <br />'- ~{-~~ <br />"-,,.q,."j/ \..._- <br />."' <br />$>""'/ <br />",I ~(i.ley <br />~'y/ ) <br />/ Grand <br />I u.ke <br /> <br />G:"nbV <br /> <br /> <br />,', <br /> <br />d <br /> <br />Figure 31. Continued. (c) 0025 GMT, 1 August 1976. (d) 0100 GMT, 1 August 1976. <br /> <br />in conjunction with surflCe observations and <br />the Table Mountain wind data, a sounding <br />was constructed for Loveland, Colorado, <br />valid at 0000 GMT. This sounding, shown in <br />Fig. 32, is an estimate of the Big Thompson <br />storm environment. The L.I. was -6, and <br />the mean vapor mixing ratio below the <br />temperature inversion was 14.8 g kg-I. <br />The LCL was at 730 mb (= 1. I km AGL), <br />which agrees with observed low cloud <br />heights at Ft. Collins, An additional 80 mb <br />of lift was necessary to bring this air to its <br />LFC. <br /> <br />3,2 Radar Coverage <br /> <br />The NHRE 10 cm radar at Grover <br />scanned the storm complex along the <br />northern Colorado foothills until a few mi- <br />nutes after 0100 GMT. During this period <br />the storm's intensity peaked about 0045 <br />G.\lT and then weakened temporarily. Re- <br />flectivity data from Limon and Grover <br /> <br />radars were compared during the peak <br />period. <br />Limon (00 elevation angle) and Grover <br />(1. 90 elevation angle) radar echoes at 0045 <br />GMT are superimposed on a map of the Big <br />Thompson area in Fig. 33. Both radars <br />scanned a section through the storms at <br />elevations between 15,000 ft MSL (4.6 km) <br />and 20,000 ft MSL (6.1 km). Limon radar <br />showed only a VIP level 3 contour, which <br />corresponds to reflectivities between 41 <br />and 46 dBZ. However, Grover radar ob- <br />served a level 5 (55-65 dBZ) with a meas- <br />ured peak reflectivity of 64,6 dBZ. The <br />Grover data contained more detail than the <br />Limon data. This is partially explained by <br />the narrower beam width of the Grover <br />radar (10 conical beam compared with Li- <br />mon's 20 conical beam) and Grover's loca- <br />tion closer to the storm area. Fig. 33 <br />suggests that Limon radar underestimated <br />the true intensity in the core of the storms <br />l;y about 15 dBi. <br /> <br />37 <br />