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<br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />~ <br />~ <br />~ <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 /> <br />Evaluation requirements for cloud seeding <br />A very daunting task <br /> <br />Methods of evaluating cloud seeding operations <br /> <br />If one were able to predict precisely the <br />precipitation from a doud system. it would be a <br />simple matter to detect the effect of artificial doud <br />seeding on thaI system. The Wor1d <br />Meteorological Organization (WMO) keeps an <br />updated Statement on the Status of Weather <br />Modification for use by its member countries. <br />This statement is written by a WMO Committee <br />of Experts (with membership from the USA) <br />and approved by the Executive Committee of the <br />WMQ, The Statement dearly indicates that. <br />although many countries around the world are <br />involved in operational projects. evaluation of <br />doud seeding effectiveness using conventional <br />methods is not acceptable. The WMO (2001) <br />comments that the expected effects of seeding <br />are almost always within the range of natural <br />variability (low signal-to-noise ratio). "Comparison <br />of precipitation observed during seeded periods <br />with that during historical periods presents <br />problems because of dimatic and other changes <br />from one period to another, and therefore is not a <br />reliable technique. This situation has been made <br />even more difficult with the mounting evidence <br />that dimate change may lead to changes in <br />global precipitation amounts as well as to spatial <br />redistribution of precipitation." The WMO (2001) <br />recommends that whenever a statistical <br />evaluation is required with cases of very low <br />signal-ta-noise ratios, "experiment durations in <br />the range of five to over 10 years may be <br />required " <br /> <br />The definition of scientific proof <br /> <br />The evidence that is required to establish that a <br />doud seeding methodology is "scientifically <br /> <br />proven~ can be divided into two aspects, namely. <br />statistical and physical evidence. Statistical <br />evidence is usually obtained by an experiment <br />based on a seeding concept (Bruinljes, 1999). <br />This experiment has to be conducted and <br />evaluated in accordance with its original design <br />using acceptable statistical methods. This <br />statistical evidence IS required to detect the <br />seeding response as specified by the conceptual <br />model. Physical evidence constitutes the <br />measurement of key links in the chain of events <br />associated with the seeding conceptual model. <br />This physical evidence is required to establish <br />that !he positive effect of seeding has been <br />caused by the seeding intervention. <br /> <br />In addition. Silverman (2001) points out that <br />experiments should be reviewed critically using <br />the proof-of-concept criteria which emphasizes <br />the results of randomized statistical experiments <br />conducted and evaluated in accordance with the <br />a priori design. Failure to satisfy these criteria <br />does not connole that seeding is ineffective; <br />rather, it simply means that the evidence was <br />insufficient to establish that seeding worked as <br />hypothesized in the original design. <br /> <br />Hobbs (2001) adds the requirement of <br />independent duplication of results before <br />conduding that any partiOJlar cloud seeding <br />technique is effective. The author also states <br />that strong statistical and physical evidence, <br />replication. and independent confirmation, are <br />stricter than those generally required in <br />meteorological research. Hobbs (2001) further <br />states that: <br />