Laserfiche WebLink
<br />~ <br /> <br />;,~) <br /> <br />-, <br />~. <br /> <br />values on semi-logar .thOlic paper. Adjustments tor depth-area were based <br /> <br />on the depth-area re' ationship presented in the NOAA publication_ Adjust- <br /> <br />ments for length of ::ecord were made on logarithmic probability paper <br /> <br />, <br /> <br />" <br /> <br />using Beard's 'table ,,[ expected probability adjustments for various lengths" <br /> <br />of record. The spatlal variation of the rainfall potential shown in the <br /> <br />Atlas for the Leftha:ld Creek basin was 'simulated by SWMl-l through the intro- <br /> <br />duction of several hyctographs. The time variat~on of the 3- and 6-hour <br /> <br />rainfall for each hyetograph was based on a study of hourly precipftation. <br /> <br />data recorded during major storms in the South Platte River basi"... -Time <br /> <br />intervals of 15- and 30-minutes were used in distributing the J- and 6-hour <br /> <br />rainfalls, respecti;vely. The 3- and 6-hour distribution is given in Table 1 <br /> <br />below. <br /> <br />TABLE 1 <br />RAINFALL DISTRIBUTION FOR J- AND 6-HOUR DURATIONS <br /> <br />3-Hour <br />End of Period <br />(Minutes) <br /> <br />6-Hour <br />End of Period <br />(l-linutes) <br /> <br />Incremental Rainfall <br />(Percent) <br /> <br />15 <br />30 <br />45 <br />60 <br />75 <br />90 <br />105 <br />120 <br />135 <br />150 <br />165 <br />180 <br /> <br />30 <br />60 <br />90 <br />120 <br />150 <br />180 <br />210 <br />240 <br />270 <br />JOO <br />330 <br />360 <br /> <br />2 <br />4 <br />4 <br />5 <br />9 <br />10 <br />40 <br />10 <br />6 <br />4 <br />4 <br />2 <br /> <br />" . <br />-",' <br /> <br />3 <br /> <br />~ <br />t::::;.- ..... <br />~" <br />~ <br /> <br />'" <br />.,':- ~., <br /> <br />{,1 <br />'., <br />','- <br /> <br />~",i <br />~ <br /> <br />~ <br /> <br />....'-.1.'. <br /> <br />-. .. 'J <br /> <br />':.":"'Y-H <br /> <br />~-'; <br />-.".....-- <br />i .,...- <br /> <br />::.T.... <br /> <br />