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<br />basin. Magnitudes start at the 3 month time scale at 0.5 (0.6) for the Yampa-White (YW) up to <br />0.9 (1.0) for the Lower Arkansas (LAR) with the dry magnitudes slightly less than the wet <br />magnitudes in parentheses. As the time scale increases for 3 months to 24 months nearly all of the <br />magnitudes have increased to greater than 1.0 which is the average annual precipitation. From 24 <br />months to 48 months time scale only small changes occur and in some basins the values actually <br /> <br />decrease. The conclusion is that the worst droughts or wet periods in Colorado are usually <br /> <br />associated with precipitation deficits or surpluses that equal or exceed the annual average <br /> <br />precipitation locally. Examination of Table 10 shows that the actual ranges are quite larger at <br /> <br />individual locations. Examination of Table 10 also reveals that the dates of the worst dry and wet <br /> <br /> <br />periods have a wide range and do not group easily into the broad time periods identified in Table <br /> <br /> <br />4. This is simply the reality of how variable precipitation is especially where convective rainfall in <br /> <br /> <br />the summer is important. A companion to Table 10 for duration of dry and wet events is given in <br /> <br />Table 11. This shows that these major dry or wet events last longer than one year and the <br /> <br />duration increases with increasing time scale. <br /> <br />Examples of the extent and severity of drought and wet events are shown on the maps of <br /> <br /> <br />Figure 12a-d. Two of the worst droughts this century were present in March 1935 (Figure 12a) <br /> <br /> <br />and September 1956 (Figure 12b). Both show more than 40% of the state in drought. Note the' <br /> <br /> <br />maps do not have areas blocked off but most higher elevations are not represented by <br /> <br /> <br />observations. There has not been such a widespread drought in Colorado at the 12 month time <br /> <br />scale since the 1950s. There is no known reason why droughts ofthis nature should not return <br /> <br /> <br />again. Two exceptionally wet periods are shown in October 1957 (Figure 12c) and June 1995 <br /> <br />(Figure 12d) for the 12 month time scale. These also have more than 40% of the state in wet <br /> <br /> <br />conditions. Each of these dry or wet periods are more extreme in a sub-portion of the state. The <br />22 <br />