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<br />I <br />'I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />II <br />I <br />I <br /> <br />'.0 <br /> <br /> <br />.0 <br /> <br />Dro,l.t colU.o" .Il' <br />Ico.'ro,l.t colli.." <br />"..hICl ..turo' <br />,roclpltoti," <br /> <br />IIlCU..It' CO"ClIltroUO" <br />of CI".t.,. frolft ....IIl. <br /> <br />4.0 <br /> <br />Clou' co"to'"I". <br />Ucaulct w.t" <br />.". ie. <br /> <br />- <br />. <br />" <br />- <br /> <br />I"cro...d COftc.ntrotlo" <br />.f cr,.t'I' frolft 'M"'" <br /> <br />I <br />:t'.0 <br />~ <br />~ <br />c <br /> <br />1.0 <br /> <br />1.0 <br /> <br />o <br />o <br /> <br />10 <br /> <br />40 <br /> <br />10 <br /> <br />100 <br /> <br />110 <br /> <br />MO <br /> <br />eo <br />. {ltlll <br /> <br />Figure 1. - Illustration of the cloud conditions giving rise to optimum <br />seeding potential. Seeding strategy is to take advantage of liquid <br />water through addition of more ice to lowl~r crystal trajectories, sweep <br />out the liquid, and minimize loss of both liquid and ice escaping the <br />barrier (from Reynolds and Dennis, 1986). <br /> <br />condensation of moisture as the moist air is forced to rise over high <br />terrain. The basic characteristics of this cloud include the following <br />(Grant and Rauber, 1985): <br /> <br />1. Vertical extent of up to several kilometers with the cloud base <br />frequently below mountain crest elevation. <br /> <br />2. Often stably stratified but may be neutral or possess small <br />pockets with weak instability. <br /> <br />3. Horizontal dimensions varying with barrier size, moisture pre- <br />sence and orthogonal windspeed. <br /> <br />4. Precipitation efficiency,.mostly dependent on temperature, <br />orthogonal windspeed, up-barrier horizontal extent of cloud, <br />secondary ice production potential and barrier slope. <br /> <br />14 <br />