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<br />~, J <br /> <br />f/l <br />~. <br /> <br />n"J':i''''7 <br />t.,.. :,..J J <br /> <br />.' ~ 1 <br /> <br />! <br />."1 <br /> <br />'.' <br /> <br />...... <br />~:::i <br />;:~ ~ <br />'-:';' <br /> <br />M E M 0 RAN DUM <br /> <br />.- <br /> <br />;:..:~ <br /> <br />To: <br /> <br />R. M. Gildersleeve <br /> <br />August 10, 1956 <br /> <br />::.' -~ <br /> <br />"j <br />~....' <br /> <br />From: J. E. Flack <br /> <br />;,. ~ <br />," <br /> <br />Subjec'~: Salvage Attributal to 'l'rnnsmountain Diversion;; at Selocted <br />Stations on tho Upper Colo.mdn !liver abov" Cameo, Colorado. <br /> <br />r~ <br />:-~.: <br />.'.-' <br /> <br />'fhis series of studies was undertaken to deterliL1.ne salvage Hater <br /> <br />b1 <br /> <br />that is attributal to transmountain diversion of Colorado River water. <br /> <br />This salvage is clue '~o reduced river stages, decreased evaporation because <br /> <br />::"',.:! <br /> <br />of less rlater surface, reduced evapo-transpiration by channel bank grow~h, <br /> <br />"'.... <br />-. -: <br />'" <br />...... <br />. .~~ <br /> <br />and reduction or elimin;rtion of over-bank fJow. 11os'~ diversions are made <br /> <br />.:;:.0. <br /> <br />!,~ <br /> <br />in such a mannEll" as to raduce high fJows of the upper Colorado River and <br /> <br />:..::) <br />" <br />.,; j <br />f <br /> <br />its tributaries. <br /> <br />Utilizing the period of water years from 1911 through 19.54, it <br /> <br />L:~ <br /> <br />..i <br /> <br />was attempted to determine tho relationship between the annual (\""ter year) <br /> <br />/~ <br /> <br />discharge, the amount of the historic transmountain diversion,ar.d the sal- <br />vage attributal to the diversion. This Wall done by analyzing the same ba- <br /> <br />:...: <br /> <br />'...; <br />,.:::: <br /> <br />sic data \dth tr'o different approaches. The basic procedure was to compare <br />the change in the l'el1ltionsh1p of Inflow and Outflow with change in trans_ <br /> <br />r,~:~ I <br /> <br />~::: <br /> <br />...... . <br /> <br />mountain diversion for a portio n of the c1rain.'1ge area of the upper Colorado <br />River. A measure of too inl'low was made by using Inflow Index Stati.ons <br /> <br />,'. <br /> <br />;:' ~ <br /> <br />.,<" (also rolled Index Supply) corrected for any transmountain dj:verf;ions above <br /> <br />". '1 the station eaee, ~.nc] compm:'c it Vl1.tl, the discharge at an OutflO\l stat1.on. <br /> <br />" <br />..... <br /> <br />......;:.1 <br />,(.8054 <br />.'. ..._".... <br /> <br />~~;<~~),;::.~;;~::-:~..l~.:i..:\:,~._.;~.:. .' <br /> <br />'/.' <br /> <br />) <br />