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<br />III. Climatic Factors <br />Streamflow and Mean Temperature: <br />Figure 1 illustrates the relationship between streamflow and temperature. The intent of Figure 1 <br />was to determine if there was a relationships between the peak flow at Cameo and mean daily <br />temperature at Glenwood Springs, as a way of estimating the timing of the spring peak flow. As <br />Figure 1 illustrates, in 1999, approximately three days after the mean temperature at Glenwood <br />Springs reached 60°F for an extended period, the flow at Cameo peaked. This trend appears to be <br />consistent with the past three water years. The data show that when the average daily <br />temperature reaches 60°F for an extended period, the streamflows peak anywhere from two to <br />five days later. <br />Figure 1 <br />1 <br />1 <br />1 <br />1 <br />1 <br />1 <br />1 <br />1 <br />1 <br />1 <br />1 <br />1 <br />'Comparison of Streamflow @ Cameo and Temperature @ Glenwood Springs <br />4000- <br />2000- <br /> r <br />0000 1 r , <br />IM <br /> <br />; <br />? i <br />1 v <br />r yr <br /> }f <br />er << <br />rr <br />4000 <br />2000 <br />0 <br />i <br />• <br />A <br />D <br />90 <br />80 <br />Flows at Cameo <br />70 -- - - - Mean Temp at <br />Glenwood Spgs. <br />W <br />LL <br />CL <br />50 m <br />id <br />400 <br />C <br />A <br />m <br />30 <br />20 <br />10 <br />0 <br />5h 198 M 7199 5121 199 501198 BM 0199 8/20/99 800199 V10199 MAM MO <br />Water Year <br />6