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<br />I <br /> <br />J H328 <br /> <br />I <br /> <br />Stochastic generation of long-term records <br /> <br />I <br /> <br />A stochastic model was used for generating long-term virgin flow <br /> <br /> <br />records for each of the five gaging stations. Records were generated for a <br /> <br />total of 50,000 years which is not excessive considering that the data were <br /> <br /> <br />generated and stored on computer. The stochastic process consisted basically <br /> <br /> <br />of generating a succession of virgin flows for each station that varied <br /> <br />randomly about the known historical means and that varied with the same <br /> <br /> <br />overall standard deviation as the historical data. The model was actually <br /> <br /> <br />more complex in that it also considered the small lag 1 auto-correlation <br /> <br /> <br />for the Poudre and Michigan rivers and preserved the cross-correlations <br /> <br /> <br />that exist between all five stations. The statistical model used was a <br /> <br /> <br />multivariate type which generated a residual matrix, preserving cross- <br /> <br /> <br />correlations, then utilized the residual to generate the flows at each <br /> <br /> <br />station. The methods used are presented in Salas et al. (Ref. 2). The <br /> <br />model for the Poudre and Michigan rivers utilized a log-normal and square <br /> <br /> <br />root-normal transformation of the data, respectively. Numerous checks were <br /> <br /> <br />performed on the generated data, and it was concluded that the long-term <br /> <br /> <br />generated records statistically matched the short-term historical records <br /> <br />quite well. A separate report was prepared describing the details of the <br /> <br /> <br />stochastic modeling process and is available in the technical addendum. <br /> <br /> <br />The generated record is too lengthy to include with this report. Five <br /> <br /> <br />traces of the Poudre River annual virgin flows, each spanning 500 years, <br /> <br /> <br />were selected from the 50,000-year record. These traces, labeled data sets <br /> <br /> <br />1 through 5, are listed as part of the technical addendum. A bar graph of <br /> <br />the Poudre River virgin flows for one of the data sets (data set 2) is <br /> <br /> <br />presented in Fig. 5. Generated data for all five of the river stations are <br /> <br /> <br />also included with the technical addendum, but only for data set 2. <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br />I <br /> <br />Comparisons to tree-ring results <br /> <br /> <br />The 50,000 years of record were generated strictly by using a stochas- <br /> <br /> <br />tic process. The results for the Poudre River were found to be quite <br /> <br /> <br />reasonable when compared to the historic record, however there were no <br /> <br /> <br />assurances that the runoff patterns observed over the relatively short <br /> <br /> <br />historic record were representative of a longer record, say the runoff <br /> <br /> <br />which occurred within the last 500 years. It was decided to use data on <br /> <br />I <br />I <br />I <br /> <br />RE:~OURCE: CON~ULT~NT~ INC <br /> <br />18 <br />