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<br />riolo~i'3 <br /> <br />. 06-19-95 Created the reservoir target file for the base scenerio as outlined in <br />the calibration procedures, For the periods prior to a reservoirs construction, I <br />used targets of zero, <br /> <br />. 06-27-95 The Maybell Mill Pipeline (440695) was only used historically <br />from about 1978 through 1983 and ran 1-2 cfs. George talked to Kent Holt <br />who-verified.that.this.structureis.noLcurrently_being_used.andjs_unlikely_to <br />be used in the future. Therefore, this structure is turned off in the model. <br /> <br />. 06-27-95 On Fortification Creek modified the proration factors on 440647 <br />and 440998 to be 0.65 and 0.35 respectively. The .xsc file in general shows too <br />much water flowing past the gauge (09246920). This is generally due to <br />upstream shortages to diversions, These shortages are due to two things, 1) <br />diversions limited by their decree, and 2) diversions shorted due to lack of <br />water in either Fortification Creek or Little Cottonwood Creek. A final set of <br />proration factors was chosen to minimize these shortages, but they still occur. <br /> <br />The percent error for gage (092469320) on Fortification Creek appears large <br />in the calibration output file, but the errors in volume are small. <br /> <br />. 06-27-95 Modified proration factors on the tributaries between Stagecoach <br />and Steamboat USGS gauges to the following: <br /> <br />walton Creek (580687) 0,67 <br />PRIEST DITCH (580830) 0.02 <br />Green Creek (580980) 0,06 <br />Morrison Creek (5B0791) 0,10 <br />Service Creek (584684) 0,06 <br />Oak Creek (5B0508) 0.07 <br /> <br />. 06-27-95 Took a look at some major divertors both in terms of quantity and <br />seniority on the Yampa mainstem and determined that for the following <br />structures, the modeled shortages were a result of diversions constrained by <br />decree, <br /> <br />L Marshall Roberts Ditch (most senior ditch in system) <br />2, WILLIAMS IRRIG DITCH <br />3, WALKER IRRIG DITCH <br /> <br />. 06-27-95 Noticed some infrequent shortages (typically one month out of the <br />study period) for the following Bear river mainstem structures (Big Mesa <br />Ditch(JUN 1990, 688 ACFT), Buckingham Mandall(MA Y 1977, 531 ACFT), <br />and Mandall (MAY 1977, 190 ACFT)) above Stagecoach that have storage <br />water in both Stillwater #1 and Yamcolo reservoirs, These shortages are due <br />to the fact that under the simulation the structures did not have the storage <br />