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<br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />3 <br /> <br />average accumulated values, The sources of data for each station <br /> <br />are documented in Appendix A. <br /> <br />It was necessary to adjust the records at three stations for use <br /> <br /> <br />in this analysis, These adjustments were as follows: <br /> <br />1. Stateline Flows - The stateline flows used in this ana- <br /> <br /> <br />lysis are the .usable stateline flows. defined by C,L, <br /> <br /> <br />Patterson of the Colorado Water Conservation Board in <br /> <br /> <br />1944 (Ref. 3, Appendix A), The usable stateline flows <br /> <br /> <br />are derived by adjusting the stateline flows to include <br /> <br /> <br />only the amounts which are within the limits derived by <br /> <br /> <br />Patterson, The daily flows are first limited to <br /> <br /> <br />divertible flows, which are those less than 800 efs <br /> <br /> <br />during the winter and 2,000 cfs during the summer, The <br /> <br /> <br />divertible flows are further adjusted to eliminate quan- <br /> <br /> <br />tities which exceed the monthly and seasonal maximums, <br /> <br />The usable stateline flows represent those flows which <br /> <br /> <br />were determined to be usable and divertible in the State <br /> <br /> <br />of Kansas at the time the Compact was negotiated. They <br /> <br /> <br />are a better indicator for evaluating potential injury to <br /> <br /> <br />Kansas than the gross stateline flows, As was antici- <br /> <br /> <br />pated by the authors of the Compact, the gross stateline <br /> <br /> <br />flows declined after the Compact went into effect, In <br />