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<br />. <br /> <br />I <br /> <br />. <br /> <br />Between October 1 and ~~y 1 follo~ing, weather conditions <br /> <br />would control canal operation. Stream flow is estinatod to be <br /> <br />divertible in the following fu~OuntS: <br /> <br />Flow availnble <br />at diversion <br /> <br />October..... . . . . . .. .. . . . . . . . . " .. . ., . . <br /> <br />10010 <br />5010 <br />75"/0 <br /> <br />December to lVlarch..................... <br /> <br />April................. . .......... .. ... <br /> <br />Flow available for stor3ge having been derived as above <br /> <br />outlined, for the perie-ds 1921-24 and 1932-37, when a reoord is <br /> <br />available at Mancos, the flow for the porio~ 1925-31 was obtained <br /> <br />by relation of storable wah,r to floo:1 flow a t Townoc as was done <br /> <br />for the Weber Reservoir. The result is shown in Table 7. <br /> <br />~~~\. <br /> <br />20 <br />