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<br />OD3188 <br /> <br />The most recent weather modification policy statement of the 10,000 member AMS (American <br />Meteorological Society), published in the March 1992 issue of the Bulletin of the AMS, indicates <br />that scientific proof remains elusive. The policy statement notes that, "There is considerable <br />evidence that, under certain conditions, precipitation from supercooled orographic clouds can be <br />increased with existing techniques. Statistical analyses of precipitation records from some <br />long-term projects indicate that seasonal increases on the order of 10 pct have been realized. <br />The cause and effect relationships have not been fully documented; however, the potential for <br />increases of this magnitude is supported by field measurements and numerical model <br />simulations." The policy statement further notes that, "The processes culminating in increased <br />precipitation have recently been directly observed during seeding experiments conducted over <br />limited spatial and temporal domains:' These brief seeding experiments which affected small <br />areas were similar to, but less comprehensive than, the direct detection experiments discussed <br />in section 4. <br /> <br />The newest policy statement of the WMO (World Meteorological Organization), affiliated with <br />the United Nations, was approved in July 1992. Both the AMS and WMO policy statements <br />were prepared by panels of experts, the latter from several countries worldwide. The WMO <br />statement notes that, "In our present state of knowledge, it is considered that the glaciogenic <br />seeding of clouds or cloud systems either formed, or stimulated in development, by air flowing <br />over mountains offers the best prospects for increasing precipitation in an economically viable <br />manner:' The policy statement notes that statistical analyses suggest 10 to 15 pct seasonal <br />precipitation increases in certain project areas. The statement continues, "Physical studies <br />using the new technology highlighted above, give convincing evidence of the production of an <br />effective seeding agent, the tracing of the agent to SL W portions of the cloud, the initiation and <br />development of ice crystals to precipitation size particles, and the fallout of additional <br />precipitation on mountain slopes in favorable situations over limited areas. Numerical <br />simulations of the process corroborate the physical studies. This does not imply the problem of <br />precipitation enhancement in such situations is solved. Much work remains to be done in <br />pursuit of the goals of strengthening the results and producing incontrovertible statistical and <br />physical evidence that the increases occurred over a wide area, over a prolonged period of time <br />and with minimum, or positive, extra area effects." The goal of the CREST is to provide such <br />statistical and physical evidence in the Basin, <br /> <br />, <br />I <br /> <br />I <br /> <br />The policy statements are markedly more positive than previous AMS and WMO statements, <br />largely because of recent direct physical evidence from a variety of new observing systems. This <br />evidence comes from a limited number of brief (1 to 3 h) experiments from a few locations as <br />discussed later. The general seeding hypothesis for winter orographic clouds apparently applies <br />to some cloud conditions, which is certainly encouraging. However, as suggested by the policy <br />statements, convincing physical evidence is needed to demonstrate that area-wide precipitation <br />can be increased in an economically viable manner over the course of several winter seasons. A <br />need to provide such convincing scientific evidence clearly exists before the emerging technology <br />will gain wide acceptance as a practical option for water resources management. <br /> <br />2.2 Overview of Past Investigations <br /> <br />Scientists have been aware of the key processes in the general winter orographic cloud seeding <br />hypothesis for decades (e.g., Ludlam, 1955). These processes are known to operate as expected <br />when meteorological conditions are suitable. Silver iodide ice nuclei will definitely create high <br />concentrations of ice crystals if introduced to sufficiently cold SLW clouds. Some of these ice <br /> <br />5 <br />