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<br />a tendency for the precipitation gradient to be steepest, increasing rapidly <br />toway'd the storm preci pitation maximum, in short-duration convective storms <br />of small areal extent. More uniiform precipitation gradients tend to be found <br />in steady-type rains and large, long-lasting storms. Expressed in terms of <br />the percentage of storm area containing 50 percent of the preci pitation <br />volume, the precipitation gradiE!nt was found to vary from 15 to 30 percent. <br />It was also found that convective raincell patterns tend to be elliptical in <br />shape. <br /> <br />Finally, the relative importance' of sampling variance and natural storm <br />preci pitat i on va ri abi 1 ity was ex.ami ned in connect i on with the eva 1 uati on <br />of precipitation augmentation ex.periments. The sample sizes required to <br />evaluate such experiments due to sampling variance alone can be appreciable; <br />however, for reasonable gage densities, it only contributes about 10 percent <br />to the total sample size requirement. Methods of obtaining reductions in <br />sample precipitation variability through the use of covariates will have to <br />be found before the use of high,~r gage network densities is warranted. <br /> <br />Acknowledgments <br /> <br />The authors wi sh to thank John 11i ddl eton and Robert Pritchard for thei r <br />assistance in obtaining the radar precipitation characteristics of Montana <br />convective storms and their statistical properties. The authors al~e also <br />indebted to Dr. K. Ruben Gabriel whose critical comments and constructive <br />suggestions led to significant 'improvements in the clarity and quality of <br />this paper. <br /> <br />25 <br />