Laserfiche WebLink
<br />ORA F T <br /> <br />~ <br /> <br />fallout of the precipitation is within a range which allows it to <br />fall into the target area. The statistical postexperimental stratifi- <br />cat 'ion 'of phys ica 1 parameters by Vardiman and Moore defined a <br />"window" which indicates when seeding would produce positive results. <br />However, routine identification of the indices requires further <br />devE!lopment for practical field use. These bounds should be refined <br />considering the specific conditions encountered at each site. This <br />redefined "window" can then be used to develop a site-specific <br />climatology of seeding opportunities. <br /> <br />~' <br /> <br />c. Treatment of Opportunity <br /> <br />After identifying a seeding window, it is essential that the window <br />be treated effectively to produce optimum results. Since the bounds <br />of (I seeding window are finite in both time and space, it is critical <br />that: any seeding system be able to introduce an effective seeding <br />material into the cloud at the appropriate time and position. There <br />are presently two categories of seeding materials and two delivery <br />techniques that have the most potential for being effective with <br />orographic clouds. <br /> <br />" <br /> <br />Seed: i ng mater i a 1 s can be categor i zed accord i ng to the method by wh i ch <br />they create ice crystals, either by heterogeneous or homogeneous <br />nucleation. Both types of seeding materials have been shown to be <br /> <br />'::1" <br /> <br />43 <br />