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<br />53.2 inches of precipitation for all seven gauges. The upper <br />curve in the figure shows that 25 percent of the episodes <br />had durations of only 1 hour, and 50 percent had durations <br />of 3 hours or less. The middle curve shows that 50 percent <br />of the precipitating hours were in episodes of 12 hours or <br />less. The bottom curve shows that half of the precipitation <br />fell in episodes of 21 hours or more which, according to the <br />upper curve, were only six percent of the episodes. The frequent <br />occurrence (90 percent) of the episodes less than half a day <br />in duration contributed 33 percent of the total precipitation <br />and were therefore of some importance, but clearly the longer <br />storms produced the most precipitation. <br /> <br />As noted above, a similar analysis was previously done <br />in the climatological analysis of the storms affecting the <br />Grand Mesa region of western Colorado. The results were generally <br />similar but it appeared that the Grand Mesa episodes were <br />of longer duration. It is also noteworthy that on the Grand <br />Mesa the shorter duration episodes (of half a day or less) <br />produced only 16 percent of the total precipitation compared <br />to 33 percent for the Arizona episodes. Conversely; the Arizona <br />episodes produced more of the total precipitation within a <br />shorter period of time than did the Grand Mesa episodes. <br /> <br />Table 3-6 offers a comparison of these two analyses, <br />where the difference in episode duration is quite evident, <br />e.g., 75 percent of the Arizona episodes lasted 7.5 hours <br />or less, while on the Grand Mesa, 75 percent of the episodes <br />lasted 14 hours or less (nearly twice as long). At the 90 <br />percent level the difference in episode duration remained <br />about the same (8 hours longer on the Grand Mesa) but 5 percent <br /> <br />3-43 <br /> <br />I <br />I <br />I <br />I <br />, <br />f <br />I <br />, <br />t <br />, <br />t <br />I <br />I <br />, <br />, <br />I <br />I <br />I <br />I <br />