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<br />'" <br /> <br />90 <br /> <br />,..,,;...--- <br />//..,;'" <br />,4/ ,..' <br />.7 ../ <br />~.// ,// <br />/' / /' <br />. /' <br />/ //"--, <br />/ // CO <br /> <br />//' <br />/ / <br />/ // <br />/ // <br />///;~ <br />'// <br />./1 <br />1/ <br />10 I <br /> <br /> <br />(}) Est/mote boJ<<1 on method in Ctark (1971) <br />([) <br /> <br />00 <br /> <br />. <br />e <br />~ 70 <br />" <br /> <br />u <br />~60 <br />. <br /> <br />Oeptlt-Ourofi()n C/JrVI of J~II(J/)r f'(Jin <br />recordM of Fort Collins 9 Miles Nit' ILaporte) <br />2215 July 31 to 01/5 AU9. 1,1976 ''''OT/ <br />o Hosed on method ill 8urI(Ju of <br />~clomoti()n (/913) <br />@) Triol Curl".' lIton of (]) ond Q) 10 <br />75:r of time, tfl,,, ([), <br /> <br />" <br />~ ~o <br />e <br /> <br />~ 40 <br /> <br />. <br />~ 30 <br />~ <br />~ <br />. <br /> <br />/ <br /> <br />81G THOMPSON R/V!R ORAINAGE <br />fOLOHAOO <br />DIMENSIONLESS DfprH-{JUHATlON CflNVES <br />THUNOERHORIr/ RAINfALl. <br /> <br />20 <br /> <br /> <br />, <br />o 2D ~ 40 ~o ~ 10 W ~o 100 <br />TilliE AS PERCfNT OF DURATION <br />F1gurl! 3. D1mensionless deptll-durat;on curves. Curve number 4 was adopted 1n this <br />study. <br /> <br /> <br />. <br />i <br />+ <br /> <br />~ <br />i <br />+--' <br /> <br />-" <br />. <br />t <br />1 <br /> <br />~00.; <br />~~. <br />~~ <br />\ <br />~ <br />w/>~ <br />:), <br />'/ry <br />::! <br />:i <br />ff <br />'t <br />~y <br />,:;- <br />c:l~ <br /> <br />I <br />J <br />fj <br />'2] <br /> <br />J~MlUlloa"""STUO'l''''''' <br />2/ <br />g <br />~ <br />?J <br />'~'~~~+__to' <br /> <br />NOTE AloIALYSISLU",UC <br />'mAltfAI'IVCl-OSH <br />IT2"tSOlo1YET <br /> <br />, <br />~--=-== <br />Sl;"~OF'''T <br /> <br />Figure 4. Isohyetal pattern derived in this study for the intense 4-hour storm period <br />from 1830 to 2230 MOT 31 July 1976. <br /> <br />138 <br />