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<br />On the basis of these observations. there were 23 days when the positive <br />rainfall anomalies were downwind from the seeding (to south and west) <br />and only 3 days when downwind was in the direction of negative anomalies <br />(north and east). Of the latter 3 days (July 19 and 20 and August 7). <br />none appears to fall in the top quintile of the daily rainfall distribu- <br />tion. and it may therefore be assumed they contributed little to the <br />pattern of anomalies. Thus the facts exactly contradict Osborn's thesis. <br /> <br />Osborn questions the possibility of making a more rigorous analysis <br />than his map of anomalies. McDonald (1969) noted that the anomaly method <br />gave way about 1952-53 for purposes of weather modification evaluation <br />to the much more powerful method of target/control regression, with this <br />and other methods undergoing progressive refinement since that time. A <br />number of evaluation procedures based on precipitation measurements at <br />the ground not involving randomization. and therefore applicable to <br />ARIDROP, have been put forward (e.g.. Howell, 1951; Nason and Lopez. <br />1967; Stidd, 1967; Elliott. 1969). There are numerous examples in the <br />open scientific literature of elegant and highly informative applica- <br />tions of such methods to rainfall data poorer than that available in <br />Arizona. <br /> <br />The Santa Catalina Experiments <br /> <br />Osborn's second grounds are inferences from experiments reportedly <br /> <br />indicating "apparent loss" of rain associated with seeding, chief 8JIOJlg <br /> <br />2 <br />