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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 />I <br />I <br />I <br /> <br />shown to have a reasonable number of days with dynamic seedability. <br />The Dulles sounding appears to give a sufficiently good estimate of <br />seedability to be used on an operational basis. <br />Radar and aircraft measurements demonstrate that the <br />characteristics of the showers are similar to those measured else- <br />where under similar meteorological conditions. We further interpret <br />that the physical response from properly seeded cells is consistent <br />with the physical response hypothesized with the dynamic seeding <br />concept. The high frequency of mid-level stable layers appears to <br />be a key factor in the determination of seeding potential. H these <br />layers are at warm temperatures (_50C) or are fairly intense, seeding <br />with AgI does not glaciate the updraft region sufficiently to provide the <br />tuoyancy needed to accelerate beyond the stable layer and produce the <br />needed vertical growth. In the cases with an unstable cloud llayer, the <br />seeding response correlates well with the physical concept. <br /> <br />124 <br /> <br />- <br /> <br />.l.... <br />