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<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 />I <br />I <br />I <br />I <br /> <br />o' <br />, <br />, \ <br /> <br />Storm RainfalV (CSR) model. CSR model output of peak storm total <br />, <br />rainfall, te~poral distribution of rainfall in 10 minute steps, storm <br />duration and peak 10-, 30- and 60-minute intensities were calculated. <br /> <br />3. The CSR model output was compared to historical rainfall records of <br />peak point storm total, intensity values and temporal distributions. <br />Comparison of model peak point rainfall for the three storms are shown <br />in Figure 5. <br /> <br />4. The temporal distribution of the CSR model peak point rainfall was <br />then applied in a proportional manner to each 0.5 inch of isopluvial <br />band in the historical rainfall surveys to obtain the temporal rain- <br />fall within each of the subbasins. Since each convective storm sur- <br />veyed covered a relatively large area, more than one CSR model run was <br />needed to cover each storm profile. <br /> <br />. -.y-'_I./ <br />\"- r,:, ~ _.\u-- ,. <br />B. \ transposition of the historic storm events over the Boulder Creek <br /> <br />watershed. <br /> <br />I. A prime consideration in the dynamic transposition of a storm event <br />over a watershed is the relationship between the winds in the sub- <br />cloud and cloud layers. The winds in the sub-cloud layer provide the <br />source of moist energy for the storm's growth. These winds establish <br />the location of the updraft within the storm. The cloud layer winds <br />strongly influence the general direction of movement of the storm. <br />~_.-___ ____~ !," .s, ....., <br />The vector:difference'of the two winds establishes the propogation or <br />", ~, <br />general movement pattern of raincells within the storm complex. In <br />essense this vector establishes the axis of ellipticity of the rain- <br />fall field. <br /> <br /> cloud <br />., tion. <br />\ basiIJ <br />I <br /> \ <br /> <br />2. Using the upper air temperature, moisture and wind field observations <br />for the storm event used in the reconstitution, the elevation of the <br />base is obtained and the degree of lift required for its forma- <br />This elevation is compared to the elevation profile of the <br />and is used to fix the elevation location of the rainfall field. <br /> <br />,-)"", <br />(/',' <br /> <br />9 <br />