Monthly point rainfalls due to a storm at rain-gauge stations A, B, C, D and E in a Waterval basin are shown in Fig. 3. Suppose the station D was not in operative for long period of time. The recorded annual rainfalls for stations A, B, C and E are 91.7, 76.2, 82.5 and 66.8 mm, respectively. 4.1. Calculate the scale of the map 4.2. Determine the average areal depth of rainfall over the basin using the: (a) Arithmetic Mean method (b) Theison Polygon Method 4.3. Estimate the annual rainfall at station D using: (a) Comparison Method (b) Normal Ratio Method km 60 C 7.2 mm 40 B 6.8 mm 75mm 20 0 Figure 3 D 7.8 mm E 6.8 mm (km)

Structural Analysis
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ISBN:9781337630931
Author:KASSIMALI, Aslam.
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Chapter2: Loads On Structures
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Monthly point rainfalls due to a storm at rain-gauge stations A, B, C, D and E in a Waterval basin are shown
in Fig. 3. Suppose the station D was not in operative for long period of time. The recorded annual rainfalls for stations
A, B, C and E are 91.7, 76.2, 82.5 and 66.8 mm, respectively.
4.1. Calculate the scale of the map
4.2. Determine the average areal depth of rainfall over the basin using the:
(a) Arithmetic Mean method
(b) Theison Polygon Method
4.3. Estimate the annual rainfall at station D using:
(a) Comparison Method
(b) Normal Ratio Method
km
60
C
7.2 mm
40
B
6.8 mm
75mm
20
0
Figure 3
D
7.8 mm
E
6.8 mm
(km)
Transcribed Image Text:Monthly point rainfalls due to a storm at rain-gauge stations A, B, C, D and E in a Waterval basin are shown in Fig. 3. Suppose the station D was not in operative for long period of time. The recorded annual rainfalls for stations A, B, C and E are 91.7, 76.2, 82.5 and 66.8 mm, respectively. 4.1. Calculate the scale of the map 4.2. Determine the average areal depth of rainfall over the basin using the: (a) Arithmetic Mean method (b) Theison Polygon Method 4.3. Estimate the annual rainfall at station D using: (a) Comparison Method (b) Normal Ratio Method km 60 C 7.2 mm 40 B 6.8 mm 75mm 20 0 Figure 3 D 7.8 mm E 6.8 mm (km)
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