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22 <br />METHODS AND MATERIALS <br />LIMNOLOGICAL CHARACTERISTICS <br />Stream Flows <br />Mean monthly and annual historic streamflow records were obtained <br />from publications of the U.S. Geological Survey on file at the U.S.G.S. <br />field office in Grand Junction, Colorado. Emphasis was placed on sta- <br />tions with the longest duration of historical records: Taylor River at <br />Almont; below the Gunnison Tunnel; and the Gunnison River near Grand <br />Junction, Colorado. Considerable time was spent during the present <br />study in calculating a hypothetical station, called "Above Gunnison Tun- <br />nel," by adding discharges that were historically diverted into the Gun- <br />nison Tunnel to the discharges recorded below the Gunnison Tunnel. <br />Means were claculated for time periods associated before and after the <br />construction of the various major structures that now exist in the <br />Gunnison drainage. Discharge data from the Curecanti reservoirs were <br />supplied by the U.S. Bureau of Reclamation Power Operation Office in <br />Montrose, Colorado. Some records were also obtained from the Uncompahgre <br />Valley Water Users in Montrose regarding discharges from Taylor Park <br />Reservoir as well as discharges into the Gunnison Tunnel. <br />Temperatures <br />In November 1971, the Bureau of Reclamation installed three continu- <br />ous recording thermographs in the Gunnison drainage. The uppermost was <br />installed below the Gunnison Tunnel in the same area that Kinnear and <br />Vincent (1967) had operated a thermograph during portions of 1965 and <br />1966, before Blue Mesa Reservoir was in full operation. A second thermo- <br />graph unit was installed in the North Fork of the Gunnison River alongside