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Last modified
7/28/2009 2:39:58 PM
Creation date
4/23/2008 12:04:56 PM
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Weather Modification
Title
The Management of Weather Resources - Volume II
Prepared For
The Weather Modification Advisory Board
Date
6/30/1978
Weather Modification - Doc Type
Report
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<br />A-I <br /> <br />A. SELECTED ISSUES <br /> <br />The issues Wl~ are about to discuss are important for at least one (more usually both) of <br />(i) how we assess Jrecent experiments and present knowledge and (iO how experiments should <br />be designed, conducted, and analyzed (beginning at once). <br /> <br />1. Basic Ideas <br /> <br />* randomization * <br /> <br />The only reliable cure to many problems of experimentation is randomization t, the use of <br />sequences of application of treatments -- here "seeding" or "not seeding" -.. that are not <br />merely seemingly unpredictable but have known (and carefully chosen) probabilities of <br />occurrence. In experiments in which people play important roles in either choice or assess- <br />ment, randomization often plays an extra role. (For instances in medicine and surgery, see Gil- <br />bert, McPeek and Mosteller, 1977 J Over the last decade or so, randomization has come to be <br />recognized as an essential part of gathering trustworthy data about weather modification.. It will <br />remain absolutely essential for the foreseeable future tl: <br /> <br />* exploratory/confirmatory/piggyback * <br /> <br />Today we realize that experiments focused on weather modification will almost inevitably <br />have to have two separate phases, each of which is likely to require several years. This is <br />because we just do not know enough, when moving from one geographic area to another, to <br />forecast reliably which weather situations are most Iik(~ly to be susceptible to seeding. Without <br />an exploratory phase, in which we obtain reasonable identification of the kind(s) of situations <br />for which seeding seems likely to work in this place and season -- and, if we are fortunate, we <br />learn how to adjust observed rainfall for other observed variables -- conducting a serious <br />confirmatory trial will usually be wasteful of both money and time. Without a confirmatory <br />phase, in which seeding under apparently favorable situations is tested under the high1est stan- <br />dards, we will never have the hard evidence that we need. <br /> <br />Both phases must be extensive enough to giv,e reasonable precision of measun:ment, <br />something usually not available in a year or two. <br /> <br />Should we continue to learn more and more about which situations are most su:scl~ptible <br />to seeding -- at least in familiar combinations of land conformation, weather patterns, and sea- <br />son -- we may come to have less need for exploratory phases. An optimist might hope that this <br />will begin to occur in five to ten years. There is no indication that this is the case today. <br /> <br />Finally, then: is the important possibility of "piggyback" experimentation, where cloud <br />seeding operations can be modified enough to allow them to also serve an experimental purpose. <br />Here the most difficult aspects lie in finding modifications that both (i) are acceptable to those <br />paying for and conducting the operations and (iO meet the necessarily high standards, including <br />randomization, that are needed if we are to be able to use the results as solid evidence. The <br /> <br />tWe admit there are occasions where randomization is not feasible, but we assert confidently (a) that thiil <br />happens less frequently than is generally believed and (b) that such exceptions do not arise in experimental <br />weather modification. <br /> <br />,tThere may be rare opportunities where natural controls or other concomitant observations (unaffected by <br />seeding) are so effectiv,e, usually under unusual circumstances and only when long periods, such as years, am <br />to be treated as wholes, that unrandomized trials make some sense. If such opportunities are found, particu- <br />lar attention should be: given to incorporating, in the planned analysis, measurable aspects of the weather <br />over both the long periods involved and large areas (such as whole or half hemispheres). <br />
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