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WSP06521
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Last modified
1/26/2010 2:23:09 PM
Creation date
10/12/2006 1:41:37 AM
Metadata
Fields
Template:
Water Supply Protection
File Number
8111.831
Description
Arkansas River Compact Administration - Article VIII (H) Investigations
Basin
Arkansas
Date
1/1/1985
Author
David Pope
Title
Supplement Report to ARCA Regarding Article VIII (H)
Water Supply Pro - Doc Type
Publication
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<br />City a~d Las Animas stream gages and is not reflected by the <br /> <br /> <br />adjusted Canon City records used in the mass diagram analy- <br /> <br /> <br />sis. The magnitude of these transmountain return flows is <br /> <br /> <br />believed to be equivalent to nearly half of the average <br /> <br /> <br />annual flow of the Arkansas River measured at Las Animas. <br /> <br /> <br />The continued existence of these return flows in the <br /> <br /> <br />Arkansas River is not guaranteed because users of transmoun~ <br /> <br /> <br />tain water are entitled under Colorado water law to reuse <br /> <br /> <br />and completely consume transmountain diversions; whether the <br /> <br /> <br />users of transmountain return flows along the Arkansas River <br /> <br /> <br />are so entitled under interstate law is not controlled by <br /> <br /> <br />Colorado law. Pursuant to Colorado law, the Cities of <br /> <br /> <br />Colorado Springs and Pueblo currently have applications <br /> <br /> <br />pending in Colorado Water Court for approval of a reuse and <br /> <br /> <br />exchange plan involving large quantities of transmountain <br /> <br /> <br />return flows. If transmountain return flows are not main- <br /> <br /> <br />tained, the future available supply for downstream users on <br /> <br /> <br />the Arkansas River would decrease significantly. This <br /> <br /> <br />decrease in supply would reduce the quantities available for <br /> <br /> <br />conservation storage in John Martin Reservoir and usable <br /> <br /> <br />state line flows. <br /> <br /> <br />It is obvious that transmountain return flows have <br /> <br /> <br />affected streamflows, particularly above John Martin <br /> <br /> <br />Reservoir. Accordingly, it is equally obvious that de- <br /> <br /> <br />pletions of flow above John Martin Reservoir are being <br /> <br /> <br />masked by transmountain return flows. It is unreasonable to <br /> <br /> <br />assume that transmountain return flows have no impact on <br /> <br /> <br />streamflows or to discount their existence as Colorado has <br /> <br />-25- <br />
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