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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 />. <br />I <br /> <br />0021Q2 <br /> <br />Hydrosphere's Colorado River Model <br /> <br />December 29, 1993 <br />Page 9 <br /> <br />Severe and Sustained Drought Hydrology <br /> <br />A hydrologic trace was developed to study the effects and possible coping mechanisms <br />during a severe and sustained drought. The trace was developed from the tree-ring <br />reconstruction of pre-historic annual flows from 1579 to 1600. This period was found to <br />contain the most severe drought in the over 500 years of tree-ring reconstructed streamflows. <br />The annual flows in this period were then re-arranged in a descending order, resulting in a <br />clustering of the extremely low flows about a single point. This configuration then produced <br />the most severe and sustained drought hydrology. The annual reconstructed flows as arranged <br />were then disaggregated over time into monthly flows at Lee Ferry, and again disaggregated <br />over space to the 29 inflow points in the Colorado River Model. <br /> <br />Indexed Sequential Hydrology <br /> <br />Two indexed-sequential traces are available with Hydrosphere's Colorado River Model. <br />With the indexed sequential method multiple traces are generated by wrapping the first five <br />years from the beginning of the historical trace to the end. This is repeated until all possible <br />sequences (16 sequences in a 78-year trace) have been generated. Each sequence differs from <br />the next only by the fact that the first streamflow year is incremented by five and wrapped to <br />the end of the sequence. A second indexed-sequential trace which increments by one year <br />rather than five is also available. These traces are provided for comparisons between CRSM <br />and Hydrosphere's Colorado River Model. <br /> <br />Hydrosphere Resource Consultants 1002 Walnut Suite 200 Boulder, Colorado 80302 <br />