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<br />Gabriel: Field Experimentation in Weather Modification
<br />
<br />K. RUBEN GABRIEL *
<br />
<br />81
<br />
<br />Comment
<br />
<br />Dr. Braham has raised the question of how deeply
<br />statisticians should be involved in weather modification
<br />work. This is an interesting question which is presumably
<br />equally relevant, mutatis mutandis, to other areas in
<br />.which statistics is used.
<br />To deal with this qu.estion, it is useful to distinguish
<br />four stages of statistical activity in the experimental con-
<br />text: (1) the experiment is designed i (2) it is performed i
<br />(3) the principal hypothesis of the experiment is con-
<br />firmed or refuted and the corresponding parameter(s)
<br />estimated; and finally, (4) other aspects of the results
<br />are explored. .The confirmatory stage (3) of analysis con-
<br />centrates on the principal purpose of the experiment, that
<br />hypothesis and/or those parameters for whose study the
<br />experiment was designed. Thus, the principal motivation
<br />of weather modification experiments usually is to deter-
<br />mine whether the hypothesis, that seeding augments pre-
<br />cipitation (the parameter), is sufficiently true to justify
<br />operational cloud seeding-the proposed action. In ad-
<br />dition, the data from such experiments are scanned for
<br />effects on distributions of precipitation, and for relation
<br />of seeding effects to season, to time, to extent of seeding,
<br />and to a host of concomitant meteorological variables.
<br />These are the exploratory analyses, which form stage (4)
<br />. of statistical activity.
<br />Few experiments are analyzed only for the single
<br />principal hypothesis, and only rarely will an "ex peri-
<br />'ment" be run just to allow undirected exploration of its
<br />results. In general, experiments are aimed at a combina-
<br />tion of confirmatory and exploratory analyses, the former
<br />relating to the principal question posed by the experimen-
<br />ter, the latter allowing him to fan out in the search for
<br />novel ideals. It is not generally useful to label an entire
<br />experiment as either confirmatory or exploratory, since
<br />most experiments allow BOrne analyses of each kind.
<br />Analysisand experimentation are a sequential or cumula-
<br />tive process. The exploration of one experiment's out-
<br />comes usually results in the formulation of new hypo-
<br />theses which may then be subject to confirmation by the
<br />next experiment.
<br />Now consider the statistical methodology appropriate
<br />to stages (3) and (4). (Planning these analyses also
<br />determines the proper design and performance of the
<br />experiment.) The confirmatory analysis stage (3) fits
<br />very well into the framework of two-decision significance
<br />testing theory. A hypothesis is formulated, variables
<br />chosen, distributions postulated, parameters defined, and
<br />
<br />· K. Ruben Gabriel is Professor of Statistics and Biostatistics at
<br />the University of Rochester~ Rochester, NY 14627.
<br />
<br />
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<br />
<br />a statistic derived so as to maximize test power and/or
<br />estimation efficiency. The experiment is supposed to have
<br />m~en performed strictly according to the design, and to
<br />culminate in the computation of a statistic which leads
<br />to a decision-all this exactly following the protocol set up
<br />in the design. The end product is a statement of signifi-
<br />es.nce, accompanied by an estimate of the relevant pa-
<br />rameter with error intervals.
<br />The exploratory stage (4) consists of all conceivable
<br />analyses of the experimental results classified in any
<br />reasonable way, with a view to verifying hunches about
<br />the special characteristics of seeding effects (e.g., rare
<br />extreme "blockbuster" effects vs. common average
<br />effects), about their relation to time (e.g., hours after
<br />seeding, month of year), to place (.e.g., within-plume or
<br />outside it, on-target or downwind), to type of storm
<br />(e:.g., wind direction), to cloud type (e.g., tower height,
<br />Wi!l.ter content, seeding nucleus prevalence), and about
<br />the relevance of any other information. Some of the con-
<br />comitants will have been suggested a priori by earlier
<br />e:xperiments, others will occur as a result of inspecting
<br />the data.
<br />The statistical methodology required for such in-
<br />vestigati~n is mainly descriptive and exploratory data
<br />analysis. Methods ~f sifting through multiple cross-
<br />cl:ilSSifications come into their own here, as do techniques
<br />for tracing trends, locating differences, and identifying
<br />J>f~tterns. Classieal methods of hypothesis testing are quite
<br />marginal to this activity. The criteria a.re not maximal
<br />power or efficiency but rather resolution of data into
<br />interpretable regularities. In exploring many facets of the
<br /><u~ta, one is very unlikely to know enough about each
<br />facet to allow selection of "optimal" techniques. Instead,
<br />one does better with simple techniques which are suffi-
<br />cil~ntly easy to understand to allow the statistician to
<br />work hand in hand with the meteorologist. They should
<br />explore experimental results together, suggesting patterns
<br />and ideas to each other and progressively sifting the data
<br />and interpreting them in physical terms.
<br />This stage of analysis is classified as exploratory be-
<br />cause that is the main thrust of any freewheeling study
<br />of an experiment's results. But exploration is always ac-
<br />companied by some confirmation (Tukey 1977, p. vii):
<br />any striking finding of the exploratory analysis will also
<br />be judged in terms of how likely it is to have arisen by'
<br />pure chance. The investigator will require something like
<br />st:!l.ndard errors or P-values to be attached to expl9ratory
<br />.findings so that he has some idea of how "nonrandom"
<br />they are. One problem with such confirmatory calcula-
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