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<br />only exception usa in 1934 when temperatures were such thet <br />the irrigation begen dl1ring April. During tb.1e month the <br />!low wall conlS1dered to be lOO% Iltoreble to t!l.e beginning <br />at the irrigation aeason. The resulting storable flovs for <br /> <br />the ~eriod of record at Jackson Gulch ere given in table 11. <br /> <br />In deter:rlning the storable !low for the IYebe'r Refler- <br /> <br />voir site during the irrigation aeDson, it was assumed thet <br /> <br />the .flo'VI at the !Seat. Mancoll divc.re10n Yiall 7.07'f, and the <br />Middle Ml\ncoll was :J.6.l6l' of the flow 81'. tM gllga, except <br /> <br />that, after the flow below the diversions lillll inadequate <br /> <br />to :;up~y u-rii>lltion, the diversion from the lUddJ.e Monaoo <br /> <br /> <br />woulcl be regulated to Ill1llU up the deficiency in supply be- <br /> <br />foro the !test lilancos, because there ill practically DO in- <br />flow be.lOll' the diversions on the Middle Uc.ncosto provide <br /> <br />for decrees on that strecm, while 'the diversion on the Enat <br /> <br />Mancos 10 high, with considerable inflow below to take cere <br />at decrees 'on it. During the remainder of the ;year, lOO~ <br />at the flow wee conaidered atorcble at both diverBions ror <br /> <br />October, 50% at both diverlllono for November, 50" on the <br />!diddle Llanco13 for December to M.r.rch inclusive, and none on <br />the EOllt Mnucolil for thllt period. For April, 75% wes con- <br />&idersd 00 ~torable on the Middle ~nc08, and none on the <br />East iklncos till the 15th, nfter which it "BS taken toe <br />100% storv.ble. Ibe resulting 6torsble flow for the periods <br /> <br />of record ere shown in table 12. <br /> <br />~ <br />o <br />o <br /> <br />52 <br />