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BOARD01635
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Last modified
8/16/2009 3:04:44 PM
Creation date
10/4/2006 6:59:44 AM
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Board Meetings
Board Meeting Date
3/26/1945
Description
Table of Contents and Minutes
Board Meetings - Doc Type
Minutes
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<br /> <br />.. <br /> <br />" <br /> <br />nd <br /> <br />,- <br /> <br />he <br /> <br />,- <br /> <br />.s <br /> <br />,rry, <br />,au <br /> <br />extent. ,Colorado says that data for drouth conditions, and suo';normal cy- <br />cles such as 19~1-194o, are important. out says that such data should ap- <br />pear separately from virgin flow estimations. Due to the uncertainties as <br />to when another such cycle of years may be encountered. and as to what then <br />may be the status of development, Color~o says th.t so-called virgin flows <br />for such an assumed dromh cyCle will 'be Jilisleading;'imd-Will not indicate <br />the streamflows available for irrigation. pcwer. and other purposes. unless <br />accompanied by reservoir operation studies to show, the effect~ of stream- <br />flow' regulation and the additional supplies of ""ter thereby made available <br />during euoh a period of years. Colorado suggests the inclusion in the Re- <br />port of such reservoir operation studie.. on virgin flow conditions to show <br />the regulating effect at Lee Ferry and the International Boundary, of mass <br />operations of reservoirs above those pointa. <br /> <br />20. Virgin flow' quantities shown in the Report are the sum of: (a) <br />the average annual streamflows recorded at (or scheduled for) the desig- <br />nated gaging station; plua (b) the allowances for upstream "depletions" <br />in the average year of the swne period. - said "depletions" being the quan- <br />tities of water estimated to have been withheld from the stream by the di- <br />I <br />version. use and storage of ""ter from and in the natural drainage basin <br />upstream from the designated station. Neither the recorded streamflows nor <br />the "depletion" allowances. of the historio period. are shmm in the Report. <br />Colorado suggests that, for two key stations, the Report. should contain <br />detailed information concerning both items; and that the key stations should <br />be, Colorado Ri Vel" at Lee Ferry and, Internati onal Boundary. <br /> <br />21. Colorado points out that since "depletions" are a part of the es- <br />tinated "virgin flows," an understanding of what is meant by "virgin flows" <br />depends in part on the meaning of "depletions. III which are defined in <br />general as the differences between diversions and returns; and that evapo- <br />ration loeses from existing and potential main-stem reservoirs are entered <br />as depletions. but are not measurable by the difference between diversione <br />and returns. A proper definition of "depletions" would include both the <br />manner of calculation, or the factora employed' in the estimations, and the <br />place of evaluation, whether at the places where such "depletions" occur. <br />- or in terms of their resulting effects at points downstream. The data <br />presented are inconsistent in this respect. and therefore are not direct- <br />lY,cornparable. Upper Basin depletione appear to have been evaluated as of <br />the places where they occur. whereae in the Boulder and Gila divisions of <br />thl! Lower Basin. the upstream "depletions" appear to have. been credited <br />with the estimated salvage of water or reductions in natural conveyance <br />losses attributable to the diminished volumes and regulated character of <br />the flows resulting from upstream development. Colorado urges that both <br />basins be treated alike. <br /> <br />22. The recorded streamfloWll at designated gaging stations are the <br />unconsumed outflows from the upstream drainage basin. that were not with- <br />held from the stream either by man-made "depletions" or by natural losses <br />of water. In oaloulating the "virgin flows" of the Report. the man-made <br />"depletions" were added to the recorded outflows. and the natural losses <br />were ignored. Thus "virgin flows" may be said to indicate the streamflows <br />that might have been recorded during the average year of a similar olimatic <br /> <br />
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