8. The annual precipitation (in mm) observed on a network of stations is shown in the figure below. Compute the average areal rainfall by: a. Thiessen polygon method. b. Isohyctal Method The scale of the figure is 1 sq.grid = 169km² (1 unit = 13km) 625 610 1010 980 T090 650 1075 720 890 750 390

8. The annual precipitation (in mm) observed on a network of stations is shown in the figure below. Compute the average areal rainfall by: a. Thiessen polygon method. b. Isohyctal Method The scale of the figure is 1 sq.grid = 169km² (1 unit = 13km) 625 610 1010 980 T090 650 1075 720 890 750 390

Structural Analysis

6th Edition

ISBN:9781337630931

Author:KASSIMALI, Aslam.

Publisher:KASSIMALI, Aslam.

Chapter2: Loads On Structures

Section: Chapter Questions

Problem 1P

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Probability, risk and uncertainty analysis for hydrological design

It gives a framework that is financially critical for finding the exceptional designs of hydrological systems with a reduced cost in total inclusive of the project cost and the disaster mitigation cost. But there would be hardly any assessment of a decent quality damage function. Hence, errors in demonstrating the hydrologic events, incorrect model parameters, and so on may occur. Here, we will discuss a specific hydrological design that of a detention basin for studying and understanding the risk-based procedure, uncertainties, and probability analysis by following a systematic framework.

Question

8. The annual precipitation (in mm) observed on a network of stations is shown in the figure below.
Compute the average areal rainfall by:
a. Thiessen polygon method.
b. Isohyctal Method
The scale of the figure is 1 sq.grid = 169km? (1 unit = 13km)
%3D
625
616
1010
980
1090
650
1075
720
890
750
390

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