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<br />occur at night downslope below snowline, and soil temperature would <br /> <br /> <br />remain colder under snowpacks and for a short distance downslope for <br /> <br /> <br />as long as the snowmelt is extended. <br /> <br />It is assumed that at high elevations an increased snowpack would <br /> <br /> <br />increase soil lOOisture levels under, and for short distances down- <br /> <br /> <br />slope of the impact point. At lowest levels on long downslopes, <br /> <br /> <br />soil lOOisture would remain relatively unaffected except along water <br /> <br /> <br />CO\ll"ses or in areas <Jf downslope accumulation such as marshes and <br /> <br /> <br />meadows. <br /> <br />It is further assumed that: <br /> <br />(1) The likelihood of accidentally triggering "superstorms" <br />is minimal" and <br /> <br />(2) No attempts will be made to seed summer storms or seed <br /> <br />early fall or late spring storms that would not ordinarily drop <br /> <br />precipitation. <br /> <br />1-5 <br />