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<br />These findings, that episode durations tended to be longer <br />in Colorado, but precipitation totals were greater within <br />shorter time periods in Arizona, may be due to the fact that, <br />in Colorado, several episodes consisted of Mesoscale Stratiform <br />(MS) cloudiness. This condition, which has been observed <br />over the Grand Mesa on many occasions, can produce long periods <br />of very light precipitation. None of these cloud conditions <br />were observed in Arizona during the field season. In addition, <br />convection, which can produce significant precipitation in <br />a relatively short time, was observed to occur in several <br />of the Arizona episodes, at least for short intervals. <br /> <br />Of the 217 episodes identified in Arizona, 152 (70 percent) <br />of them had durations of 6 hours or less with these 152 episodes <br />accounting for 395 precipitation hours. However, they only <br />accounted for 11 percent of the total precipitation. Only <br />7 percent of the 152 episodes had precipitation totals of <br />0.10 inch or more with the greatest being 0.375 inches during <br />a 5 hour period. Over a third of these episodes (34 percent) <br />had durations of only one hour, while well over half of the <br />episodes (56 percent) lasted two hours or less. Average precipi- <br />tation per gauge per episode for these short term periods <br />was only 0.04 inches while the average duration for all episodes <br />6 hours or less was 2.5 hours (median 2 hours). <br /> <br />In light of the above statistics, it may be that enhancement <br />of precipitation during these short term durations will not <br />produce significant increases in precipitation over a watershed <br />because of the small amounts of precipitation that are likely <br />to be encountered. However, as noted earlier, episodes that <br />last up to 12 hours do contribute as much as 33 percent of <br /> <br />3-45 <br /> <br />I <br />, <br />I <br />I <br />I <br />t <br />I <br />I <br />t <br />I <br /> <br />,~ <br />I <br />I <br />I <br />, <br />, <br />I <br />I <br />i <br />I <br />