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<br /> <br />The Paleohydrologic Record <br /> <br />Our gage record is relatively recent. There was no gage at Lee Ferry until 1921. In the Upper <br />Basin the longest serving big river gages are the Green River at Green River, Utah which has been <br />in place since 1894 and the Colorado River near Cisco, Utah gage, 1913 to present. <br /> <br />As noted by a number of hydrologists, our stream flow records and thus reconstructed <br />natural flows before 1930 are relatively crude.15t Reclamation and others have used a number of <br />methods, primarily statistical correlations, to reconstruct the record. The limited gage records are not <br />the only problem. Knowing the amounts of lands under irrigation and crops being irrigated is also <br />necessary to reconstruct natural flows. These records are also less reliable, the farther we go back. <br />The bottom line is that we must recognize that much of the so-called gage record is actually a <br />synthetic record with considerable uncertainty. <br /> <br />In March 1976 Charles Stockton and Gordon Jacoby published "Long-Term Surface-Water <br />Supply and Stream Flow Trends in the Upper Colorado River Basin." The Stockton and Jacoby <br />report was one of a number of studies funded by the National Science Foundation. The effort was <br />called the Lake Powell Research Project. <br /> <br />Stockton and Jacoby used dendrochronology to reconstruct a longer term (1512 to 1961) <br />hydro graph of the Colorado River at Lee Ferry.152 The report concluded that the long term natural <br />flow at Lee Ferry was only 13.5 maf + .5 maf. The Stockton and Jacoby reconstructions were used <br />for the Severe and Sustained Drought on the Colorado River Project. The results of this project were <br />published by the Water Resources Bulletin, Journal of the American Water Resources Association, <br />October 1995.153 <br /> <br />After the Stockton Jacoby report there have been a number of additional tree ring based <br />reconstructions. Most recently, in 2006 Connie Woodhouse, Stephen Gray and David Meko <br />published "Updated Stream Flow Reconstruction for the Upper Colorado River Basin" in 2006.154 <br /> <br />The January 2007 National Academy of Sciences report has a good discussion on <br />uncertainties in stream flow reconstructions. 155 The report concludes that despite the differences, all <br />of the reconstructions share important and common conclusions: <br /> <br />1. The long term average natural flow at Lee Ferry is less than the USBR 1905-2000 <br />natural flow data base. The means are in the 13.0 maf/year to 14.7 maf/year range. <br /> <br />151Tipton & Kalmbach, page 9. <br /> <br />152 A detailed discussion of dendrochronology is found on pages 11-17 of the Stockton and Jacoby report. The bottom line is that the <br />statistical methods used in dendrochronology are no different and probably more sophisticated than the methods used to recreate the <br />USBR natural flow data base. <br /> <br />153Unfortunately, the report was published during a very wet period and did not receive the attention it deserved by policy makers. <br />Copies of the journal can be obtained from Hydrosphere Inc. ",,"\\w.hvdrosphere.com <br /> <br />154The paper was published by Water Resources Research, Volume 42, January 2006. <br /> <br />155National Academy of Sciences, pages 75-76. <br /> <br />Page -68- <br />