The initial infiltration capacity in Horton model is higher for wet soil compared to that of L dry soil. 2. Interflow is the flow that reaches a stream from groundwater. T 3. The Thiessen polygon is a descriptive term for the shape of a hyetograph. 4. An increase in the relative humidity decreases evaporation. 5. When a lake is deep then the rate of evaporation decreased. 6. Manning's equation is one of the indirect methods commonly used to determine discharge.
The initial infiltration capacity in Horton model is higher for wet soil compared to that of L dry soil. 2. Interflow is the flow that reaches a stream from groundwater. T 3. The Thiessen polygon is a descriptive term for the shape of a hyetograph. 4. An increase in the relative humidity decreases evaporation. 5. When a lake is deep then the rate of evaporation decreased. 6. Manning's equation is one of the indirect methods commonly used to determine discharge.
Chapter2: Loads On Structures
Section: Chapter Questions
Problem 1P
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Transcribed Image Text:-Answer the following questions by True or False:.
- The initial infiltration capacity in Horton model is higher for wet soil compared to that of L
dry soil.
2. Interflow is the flow that reaches a stream from groundwater. T
3. The Thiessen polygon is a descriptive term for the shape of a hyetograph.
4. An increase in the relative humidity decreases evaporation.
5. When a lake is deep then the rate of evaporation decreased.
6. Manning's equation is one of the indirect methods commonly used to determine
discharge.
A storm with 10 cm precipitation a direct runoff of 5.8 cm given the time
distribution of the storm as below. Estimate the index and ealculate the rainfall
B:
excesses of the storm.
Time (hr)
2
4
7.
Rainfall (cm) 0.5
0.9
1.5 2.3 1.8 1.6
1.0 0.5
6.
3.
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