A watershed with approximately 480 acres has the time-area relationship between its sub-basins and the outlet as shown in Table 1. Direct runoff calculated using the Time-Area method for a rainfall...


A watershed with approximately 480 acres has the time-area relationship between its sub-basins and<br>the outlet as shown in Table 1. Direct runoff calculated using the Time-Area method for a<br>rainfall event is given in Figure 1. The o index of 0.5 in/hr and a depression storage of 1 ir<br>be assumed. Considering that the gross rainfall rate was always more than or equal to the in.<br>1/P<br>rate,<br>a) calculate and plot the excess rainfall hyetograph and the gross rainfall mass curve, and<br>b) estimate the lag-time and the time of rise.<br>400<br>Table 1: Time-area relation<br>340<br>300<br>300<br>Time<br>Area<br>(hr)<br>(ас)<br>200<br>1<br>70<br>200<br>180<br>2<br>200<br>105<br>3<br>180<br>100<br>1<br>3<br>4<br>Time interval (hr)<br>Direct runoff (cfs)<br>

Extracted text: A watershed with approximately 480 acres has the time-area relationship between its sub-basins and the outlet as shown in Table 1. Direct runoff calculated using the Time-Area method for a rainfall event is given in Figure 1. The o index of 0.5 in/hr and a depression storage of 1 ir be assumed. Considering that the gross rainfall rate was always more than or equal to the in. 1/P rate, a) calculate and plot the excess rainfall hyetograph and the gross rainfall mass curve, and b) estimate the lag-time and the time of rise. 400 Table 1: Time-area relation 340 300 300 Time Area (hr) (ас) 200 1 70 200 180 2 200 105 3 180 100 1 3 4 Time interval (hr) Direct runoff (cfs)

Jun 11, 2022
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