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PROJ00441
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Last modified
11/19/2009 11:43:25 AM
Creation date
10/5/2006 11:55:35 PM
Metadata
Fields
Template:
Loan Projects
Contract/PO #
C153459
Contractor Name
Loveland, City of
Water District
0
County
Larimer
Bill Number
XB 99-999
Loan Projects - Doc Type
Feasibility Study
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<br />I <br />I <br />I <br />I <br />I <br /> <br />4.3.2 Augmentation Results <br /> <br />I <br />I <br />I <br />I <br /> <br />The correlation coefficient is a measure of the consistency of the <br />relationship between two sets of data. A correlation coefficient of :1.0 <br />indicates a constant, "ideal" relationship. (In hydrology studies, this <br />occurs only in examples such as that presented earlier.) A previous study <br />for the City of Fort Collins, Colorado revealed that the annual native <br />flows of the Cache La Poudre River were highly correlated with those of the <br />Big Thompson River, with a correlation coefficient of 0.925 (RCI 1985). <br />Monthly native flow values for the Cache La Poudre were provided to CDM by <br />the City of Fort Collins for the period from 1936 to 1983 and were used in <br />this analysis to estimate streamflow values in the Big Thompson River as <br />part of the augmentation process. <br /> <br />I <br />I <br />I <br /> <br />Correlation analyses of native flows in both rivers revealed that the <br />monthly correlation ranged from a low of 0.26 in March to a high of 0.94 in <br />July. The annual correlation coefficient weighted by the average monthly <br />native flows of the Big Thompson was 0.82; this value indicates a good <br />statistical agreement between the two sets of streamflow data. <br /> <br />I <br />I <br /> <br />Precipitation data were available from 1907 to 1984. However, evaluation <br />of the augmentation analysis indicated that use of the precipitation data <br />would not satisfactorily preserve the serial correlation of monthly flows. <br />The serial correlation indicates the tendency for a "dry" June to be <br />followed by a "dry" July, etc. Consequently, precipitation data for the <br />three weather stations were used primarily to augment the record during the <br />period from 1927 to 1984 for months in which gauge data were missing or in <br />which Cache La Poudre native flows were unavailable. Correlation between <br />monthly precipitation at the various stations and monthly streamflow was <br />rather low; the maximum monthly correlation coefficient was 0.21. <br /> <br />I <br />I <br />I <br />I <br /> <br />Table 4-2 summarizes the monthly statistics of the historic and augmented <br />flow records. The standard deviation represents the dispersion of the data <br />around the mean values. The larger the standard deviation, the more <br /> <br />4-7 <br /> <br />I <br />
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