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<br />storm depends on the basin time of concentration, i,e" the travel time from <br />the upper portions of the basin to the point of interest farthest <br />downstream, The overall duration is dictated by the purpose of the estimate <br />and the importance of total runoff volume in the use of the design flood, <br /> <br />Rainfall frequency curves are derived from TP 40 (twiSr 1961), or other <br />appropriate source, for durations of 1, 3, 6, 12r and 24 hours, The values <br />are adjusted for annual series, since the TP 40 charts are for. partial <br />duration series, For a selected storm frequency, rainfall depths are <br />determined for each duration at desired time intervals and incremental depths <br />computed. If durations greater than 24 hours are needed TP 49 (NWS, 1964) <br />can be used. If the desired unit hydrograph interval is less than 30 <br />minutes, the peak 3D-minute rainfall period is incremented using the <br />following: <br /> <br />a. <br /> <br />for the peak 15 roin use 0.72 of peak 30 min :rainfall, <br />for the peak 10 min use 0,57 of peak 30 min rainfall, <br />for the peak 5 min use 0,37 of peak 30 min rainfall, <br /> <br />b, <br /> <br />c. <br /> <br />The rainfall values from the maps represent pDint rainfall. However, <br />the average rainfall over a given area will be less than the maximum point <br />value in the area, Figure 4.2 gives the reduction in the point value for <br />various precipitation durations as a function of area size, <br /> <br />~ <br />w <br />~ PO <br />Z <br />w <br />> <br />" <br />'" <br />o <br />~ <br />J 80 <br />... <br />~ <br />z <br />< <br />" <br />!z '" <br />o <br />~ <br />~ <br />o <br />!z <br />w <br />u eo <br />'" <br />'" <br />.. <br /> <br />'00 <br /> <br /> <br />l-H" RAINfALL <br /> <br />2"-H1'I RAINFALL <br /> <br />U.~HR RAINFALL <br /> <br />6-HR RAINFALl <br /> <br />3-HR RAINFALL <br /> <br />2.-"" RAINfALL <br /> <br />Weather Bureau Technlcol Poper No. 40 <br /> <br />80 <br /> <br />I~O LOO <br />AREA (Iquo,. miles) <br /> <br />80 <br /> <br />o <br /> <br />100 <br /> <br />.00 <br /> <br />"0 <br /> <br />"0 <br /> <br />400 <br /> <br />4.2, Adjustment of Rainfall Data for Area <br />22 <br /> <br />e <br /> <br />e <br /> <br />e <br />