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<br />.: ':" <br /> <br />(' <br /> <br />( <br />("- <br /> <br />c <br /> <br />( <br /> <br />"';';'; <br /> <br />~'.. <br /> <br />, <br /> <br />l:', <br />- I.' <br /> <br />l <br /> <br />RIVER =-ll!IE LINE <br />PLUS ONE-DAY CONC FLO~ GUNNISON RIVER <br />~du. ~?ak- <br /> <br />I UN IT <br />0. <br /> <br />~~**~**..~**W***W**..***n******~* <br /> <br />* FLOOD FLOW FREQUENCY ANALYSIS * <br />* VERSION DATE FER 9. 1982 . <br />. AFTER tlULLETIN I1B. SEPT 1961 . <br /> <br />**__*W***_***w**********__****._* <br /> <br />..TITLE CAROlS).. <br />TT STATION 1635 - ~O <br />TT TO COLD RI NR CAMEO <br /> <br />.."'OB CAROlS).. <br />IPPC ISKFX <br />"'1 2 1 <br /> <br />/93 1./ .. f:;-, <br />IFMT <br />o <br /> <br />IPROUT <br />52 <br /> <br />nlYR <br />o <br /> <br />..STATION IDENTIFICATION.. <br />10 1635 COLa RIVER NR STATELINE, 1934-85 <br /> <br />..SYSTEMATIC EVENTS.* <br />52 EVENTS TO BE' ANALYZED <br /> <br />.. <br /> <br />I SMR Y <br />Q , <br /> <br />IPNC!i <br />O. <br /> <br />IHE:G <br />o <br /> <br />..END OF INPUT DATA.. <br />ED +++++++++++++++++++++++++++..++++++++++++++++++++++++++++++.+ <br />+++++++++++++++++++++++++-+++++++++++++++++++++++++++++++++++++++ <br /> <br />-SKEW WEIGHTING - <br /> <br />- ---- -----...-- ---- -- ---- - _.- --- ---- _.- ---~.. -- -----.... ..~--- ------ - - ----- <br /> <br />BASED ON 52 EVENTS, MEAN-SQUARE ERROR OF STATIClN SKE:W :-99.000. <br />DEFAULT OR INPUT MEAN-SQUARE ERROR OF GENERALIZED SKEW -:: 0.302 <br /> <br />_ _ ___ _____...________ ______._________._ _...._4.._________._....______________ <br /> <br />PRELIMINARY RESULTS <br />-FREQUENCY CURVE- 1635 <br /> <br />COLO RIVER NR STATELINE. 1934-85 <br /> <br />*************************..************~*******~***************** <br /> <br />*........FLOW.CFS........* <br />* EXPECTED . EXCEEDANCE <br />* COMPUTEO PROBABILITY. PROBABILITY <br /> <br />* <br /> <br />....CONFIDENCE LIMITS.... <br /> <br />* <br /> <br />· 0.05 LIMIT 0.95 LIMIT. <br /> <br />. <br />. <br /> <br />.. ---------....-------- -- ---- *--------- --~.. *------... ..--- ----- --- ---- * <br /> <br />. <br />. <br /> <br />76-\00.. <br />72200 .. <br />68500.. <br />64200.. <br />59300.. <br />51-\00.. <br />43900" <br />30400.. <br />19200" <br />14500" <br />11200.. <br />6580" <br /> <br />* <br />. <br /> <br />*++++++++++++++++++++++++.+++++++++++++++++++++++++++++++++.++++* <br /> <br />. <br /> <br />78500. <br />13900. <br />69900. <br />65400. <br />60100. <br />51900. <br />44200. <br />30400. <br />19000. <br />14200. <br />10800. <br />6050. <br /> <br />0.002 <br />0.005 <br />0.010. <br />0.020 <br />0.040 <br />0.100 <br />0.200 <br />0.500 <br />0.800 <br />0.900 <br />0.950 <br />0.990 <br /> <br />. <br /> <br />. <br /> <br />. <br />. <br />. <br /> <br />961(10. <br />900010. <br />846010. <br />186 CIO . <br />7HC10" <br />609C10. <br />510C10. <br />34300. <br />217CI0. <br />lGHIO. <br />13:500. <br />8:500. <br /> <br />. <br />. <br />* <br />. <br /> <br />. <br />. <br />. <br /> <br />* <br /> <br />. <br />. <br />. <br />* <br /> <br />* <br />. <br /> <br />. <br /> <br />. <br />. <br /> <br />. <br /> <br />* <br /> <br />. <br />* <br />* <br /> <br />" <br /> <br />. <br />* <br /> <br />. <br /> <br />FREQUENCY CURVE STATISTICS <br /> <br />. <br /> <br />STATISTICS BASED ON <br /> <br />64100. * <br />60900. . <br />58100. . <br />54900. . <br />51100. .' <br />44800. . <br />3810 O. . <br />21100. * <br />16600. . <br />12100. . <br />9000. . <br />4820. * <br /> <br />*--------------------------------*-----------------------------* <br /> <br />" <br /> <br />MEAN LOGAR ITHM <br />STANDARO DEVIATION <br />COMPUTED SKEW <br />GENERALIZED SKEW <br />ADOPTED SKEW <br /> <br />* HISTORIC ~VENTS <br />. HIGH OUTLIEflS <br />. l.OI~ OUTLIERS <br />" ZERO OR MISSING <br />~ SYSTEMATIC ~V~NTS <br /> <br />~.'t5'+'+ <br />Q. 2230 <br />-0.8136 <br />-99.0000 <br />-a.Boao <br /> <br />. <br /> <br />. <br />. <br /> <br />. <br /> <br />o <br /> <br />. <br /> <br />Q <br />o <br />Q <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />52 <br /> <br />. <br />