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<br />. <br />II <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />~ <br />~ <br />~ <br />~ <br />~ <br />~ <br />~ <br />~ <br />~ <br />~ <br />. <br />. <br />. <br />. <br />. <br />. <br />I <br />I <br />I <br />. <br />, <br />, <br />, <br />I <br />I <br />I <br />I <br />I <br /> <br />snow water con lent and precipitation back to above average in portions of the target area. <br />However. the northern and central portions of the Gunnison River Basin received less <br />precipitation. As a consequence. water year precipitation (and in some cases snow \'..ater <br />coment) remained below a\"erage. Then. an unusually \\'ann, dry March resulted in a substantial <br />amount of sno.....melt for so early in the season. mehing as much as half or more of the snowpack <br />below about the 9.500-ft level. A couple of storms in early April added to the snowpack. <br />although both snow waler content and water year precipitation remained below normal as of <br />April 15. the end of the seeded season. Figures 3.1 to 3.3 show snow water content and <br />precipitation. and nannals. at three S~OTEl sites for the 2003-2004 winter season. It can be <br />observed from these figures that the precipitation, and in two cases, snov,:pack water content, <br />increased by 3"-5" during the first two weeks of April. It turned out that the most seeding on any <br />storm during the winter occurred on the April 9.10 storm. <br /> <br />3,1 Opt'ralional Proct'durt's <br /> <br />In operational practice, an approaching storm was monitored at the NA we operations <br />center in Salt lake City, utilizing online weather information. If the storm met the seedability <br />criteria presented in Table 2.1. and ifno seeding curtailments or suspensions \\'cre in efTect, an <br />appropriate array of seeding generators was ignited and adjusted as conditions required. Seeding <br />continued as long as conditions were favorable and precipitating clouds remained over the target <br />area. In a normal sequence of events, certain generators \\.'ould be used in the early period of <br />storm passage. some of which might be turned ofT as the wind direction changed. with other <br />generators then used to target the area in response to the evolving wind pattern. Thc wind <br />direction during productivc storm periods in Gunnison County usually favors a westerly or <br />southwesterly direction, so that the generator sites on the wesUsouthwest side of the target areas <br />were used most often. <br /> <br />l~ <br />