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Last modified
7/14/2011 11:24:22 AM
Creation date
1/18/2008 1:00:58 PM
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Publications
Year
2007
Title
The Colorado River The Story of a Quest for Certainty on a Diminishing River
CWCB Section
Administration
Author
Eric Kuhn
Description
The Colorado River The Story of a Quest for Certainty on a Diminishing River
Publications - Doc Type
Other
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<br />"i <br /> <br />The Colorado River Basin can be naturally divided into two major basins; an upper basin and <br />a lower basin. It is often described as an hourglass with the neck being the river section before it <br />enters the Grand Canyon near the historic site of Lee's Ferry. The upper river drains the high <br />mountains that rim the upper basin and the high mesas and plateaus in between. The lower river <br />begins as the river enters the Grand Canyon and runs to its mouth in the Gulf of California. The <br />upper and lower river basins can be further divided by their major tributaries. <br /> <br />Lower Basin Tributaries <br /> <br />The Gila River is the major tributary on the lower river. It drains over 53,000 square miles <br />of central and southern Arizona and western New Mexico.22 While it is a very large drainage area, <br />the Gila River System watershed is primarily desert. Almost all of the runoff originates on a very <br />small portion of the watershed along the Mogollon Rim and the White Mountains. The Mogollon <br />Rim runs from central Arizona south and eastward into New Mexico. The elevation ranges from <br />6,000' to 8,000'. The White Mountains in eastern Arizona and western New Mexico have a handful <br />of peaks that exceed 10,000'. The Gila River is a "wasting" river. In 1947, Reclamation estimated <br />that the natural flow of the Gila River at its confluence with the Colorado River near Yuma was <br />1,272,000 afper year.23 Because the study period was 1897-1943, this is probably a high estimate. <br />Other studies have suggested a natural flow more in the range of 900,000 afper year.24 <br /> <br />However, the estimated natural flow of the Gila River as it enters the Phoenix, Arizona area <br />for that same 1897 to 1943 period is 2,280,000 af per year, over a million acre feet more that its flow <br />at the mouth.25 Thus, as it flows from Phoenix to its mouth, it naturally loses over a million acre feet <br />of water. <br /> <br />Although it may contribute a relatively small portion of the flow of the Colorado River at its <br />mouth, the Gila River is the most politically sensitive and difficult tributary of the Colorado River. <br />In all but the very wettest months of rare years the Gila River is completely used and no water makes <br />it past the Phoenix area, let alone all the way to Yuma.26 <br /> <br />The Gila River system is almost exclusively used in Arizona with a little bit of use in New <br />Mexico. While the issue of how much water Arizona uses upstream versus the amount that would <br />"waste away" if it were not being used may seem like trivia, it is at the very heart of the unresolved <br />legal issues still simmering within the Basin. The Gila River was Arizona's primary motivation for <br /> <br />22House Document 419, page 172. <br /> <br />23House Document 419, TABLE CXL VI, page 284. <br /> <br />24House Document 419 estimates the virgin flow of the Colorado River at 16,270,000 afat Lee Ferry for the same 1897-1943 period. <br />(See TABLE CXL, page 281). <br /> <br />25See footnotes #7 and #8. Again, this estimate is probably high based on the 1897 to 1943 period of record. <br /> <br />26The USGS website, http:/waterdatausgs.gov. Look at the historic flows for the Gila River below Painted Rock and the Gila River <br />near Dateland, Arizona <br /> <br />Page -11- <br />
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