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• 120 <br /> h 3/1-r�r ratios. The geographical distribution <br /> with -g correlated with magnitudes of <br /> of than storms Angeles and San Diego <br /> the 16/1-h to 1-hr of fig also 4.7. Forvexample, Los Ang 0.60) <br /> the 6/1-hr ratios of figure 4.7• (approximately(high 6/1-hr ratios) have low 15-mir. to 1-hr ratios ( pP <br /> 15-min to 1-hr ratios in Arizona and Utah (low 6/1-hr ratios) <br /> were r <br /> whereas generally higher her (approximately 0.75) . <br /> for 1 <br /> ation relations for durations less than rehour were etthen smoothed <br /> Depth-duration to some of the <br /> to provide a family of curves consistent with was necessary <br /> to 6 hours, as shown in figure 4.3. Adjustment <br /> provide smoother relations through the common point at 1 hour. <br /> curve s to P <br /> justified in reducing the number of the curves shown in <br /> We believe we were ] letting one curve apply to <br /> range of 6/1-hr for durations less than corresponding curves have been indiccated amount <br /> range of s/gna ratios. The come 4 3. As an example, for any <br /> letter designators, A-D. on figure 2 <br /> between 1157 and 1352 of 1-hr, 1-mi2 (2.6-km ) s <br /> "B" . <br /> F . the associated values <br /> less than 1 hour are obtained from the curve designated as <br /> for durations pMP for selected <br /> percent of 1-hr 4.3. <br /> Table rain ratio durTheseavaluesaweresinterpolated from figure <br /> 6/1-hr rain ratios. or table 4.4) and the <br /> To determine 6-hr Pte for a basin, use figure 4.3 <br /> geographical distribution of 6/1-hr ratios given in figure 4.7. <br /> PM?4.4.--Durational variation of 1-m12 (2.6-km2) <br /> in percent of 1-hr PMP (see figure 4.3) <br /> Duration (hr) 4 5 6 <br /> ratio 3/4 1 2 3 <br /> 1/4 1/2 110 <br /> ratio ' 110 110 <br /> 93 97 100 107 109 119 120 <br /> 1.2 86 95 100 110 115 118 130 <br /> 74 89 114 121 125 128 <br /> 1.2 89 95 100 137 140 <br /> 1.3 74 118 126 132 150 <br /> 63 83 93 100 121 132 140 145 <br /> 1.4 83 93 100 147 154 160 <br /> 1.6 63 87 100 124 138 180 <br /> 1.6 43 70 130 149 161 171 <br /> 43 70 87 100 137 161 175 188 200 <br /> 1.8 70 87 100 <br /> 2.0 43 <br /> 4.5 Depth-Area Relation <br /> (2.6 km2) .. <br /> 2 PMP should <br /> We have thus far basin,developed local-storm edeterminef an PM based <br /> To apply PMP to a basin, we need relat <br /> decrease with increasing area. We have adopted depth-area <br /> on rainfalls in <br /> the Southwest and from consideration of a model thunderstorm. <br /> to <br />