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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 />56 <br /> <br />seeding th~ dissipation stage. <br />2. Discussion of the statistical experiment <br /> <br />This picture predicts a positive effect for unstable stages and no effect <br /> <br />for stable stages, so the net effect should be a positive seeding effect. <br /> <br />This \vas not observed in the San Juan proj ec t. However, not all storm stages <br /> <br />\vere seeded. Instead, only those storm periods were seeded during Hhich it <br /> <br />Has forecast that the 500 mb temperature Hou1d be -23C or warmer. (See <br /> <br />Hjermstad, 1975, for a more exact specification of the seeding criteria, <br /> <br />\oJhich varied some\oJhat over the five year period.) Since the early stable <br /> <br />and neutral stages of the storm had Harm 500 mb temperatures relative to <br /> <br />the later unstable stage, the requirement that the 500 mb temperature be <br /> <br />warm tended to favor the stable and neutral stages over the unstable stages. <br /> <br />HO\oJever, as the 500 mb temperature cooled the cloud top temperature warmed, <br /> <br />so that the cases Hith the \oJarmest cloud top temperatures were excluded. <br /> <br />More importantly, these criteria tended to exclude the more seedable unstable <br /> <br />stages and to include the unseedable stable stages in the statistical experiment. <br /> <br />The statistical experiment was diluted by including large numbers of <br /> <br />stable, unseedable storm stages, and also by the phenomenon of carryover <br /> <br />seeding. We observed (as did Hobbs et a1. 1975), that the AgI often remained <br /> <br />in the experimental area for 12 hours or more after the generators Here <br /> <br />turned off, because of the pooling of the AgI ahead of the mountain range <br /> <br />under blocking flow conditions. This led to the release of AgI into storms <br /> <br />considerably after the seeded period, and nominally unseeded storms were in <br /> <br />fact often seeded. <br /> <br />The effects cited above should lead to a dilution of the statistical <br /> <br />experiment, but not to a null effect. The arguments presented here are not <br /> <br />meant to imply that the seeding technique should not have worked, but only <br /> <br />that the statistical experiment wis seriously weakened by the inclusion of <br />