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<br /> <br />e <br /> <br />HISTORIC DIVERSIONS <br /> <br />I Intake Canal River Diversions <br />Mode <br />-- <br /> <br />The Model Intake Canal diversions from the Purgatoire River are <br />red by a ten foot Parshall flume located approximately 1,200 feet <br />measu <br />below the headgate facilities at the Purgatoire River. Much of the <br />flow in the canal at the Parshall flume is diverted into the Johns Flood <br />Ditch at a point approximately 2.3 miles below the flume. The diversions <br />into the Johns Flood Ditch are then measured separately. The Model <br />Ditch diversions, as recorded by the water commissioner, are the Model <br />Intake Canal flume measurement less the Johns Flood Ditch flow measure- <br />ment. <br /> <br />e <br /> <br />In order to obtain an extensive period of water diversions by the <br />Model Ditch, the water cornmissionerls daily diversion records were summa- <br />rized on a monthly basis for the period of 1950 through 1976 as shown <br />in Table V. Average annual diversions amounted to 7t627 acre-feet with <br />a maximum of 28t963 acre-feet in 1961 and a minimum of 625 acre-feet in <br />1975. The Model Intake Di tch diverted less than the average amount for <br />17 out of 27 years. As expected the Model In~ke Canal river diversions <br />vary drastically from month to month and year to year because of legal <br />limitations. The 1908 decree for the Model Ditch is very junior and <br />diversions were only permitted during times of high river flows and <br />during the winter non-irrigation season. <br /> <br />Model System Intercepted Runoff <br /> <br />e <br /> <br />As stated previously the Model Intake Canal, Model Reservoir, and <br />Model Ditch intercept runoff from several arroyas. This water was not <br />measured and therefore it was necessary to estimate the quantity of <br />intercepted runoff. This was done by examining precipitation records <br />and runoff indicated by the Frijole Creek stream gaging station. Since <br />precipitation events (thundarstorms) are frequently quite localized it <br />was also necessary to exercise judgment by comparing the predicted runoff <br /> <br />12 <br /> <br />-- <br />