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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 /> <br />recurrence intervals. However, deficits will occur in the 2000-high <br /> <br /> <br />scenario at the 100- and 200-year intervals and in the 201S-moderate and <br /> <br /> <br />201S-high scenarios at all four intervals. <br /> <br />Loveland's two primary sources of water - runoff from the Big Thompson <br />River watershed and the Upper Colorado River Watershed - are located on <br />either side of the Continental Divide. The impacts of a drought in one <br />watershed may be offset by the fact that the other is experiencing a normal <br />or "wet" period. This factor contributes significantly to Loveland's <br />ability to meet its future and current water demands in the scenarios <br />described above and should be remembered when considering the surplus or <br />deficit estimates for each drought interval presented in the following <br />Tables 9-2 through 9-9. A 2S-year event with respect to the total water <br />supply could be brought about by a variety of combinations in the <br />individual watersheds. <br /> <br />The contributions from each of the individual sources as shown in Tables <br />9-2 through 9-9 represent a typical mix of the available supplies but other <br />combinations of available supplies which produced similar net surpluses, <br />and/or deficits were observed in the simulation. <br /> <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />9-6 <br />