Difficulty: Easy
Correct Answer: All the above.
Explanation:
Introduction / Context:
The unit hydrograph (UH) is a cornerstone of catchment hydrology. It represents the direct runoff hydrograph (DRH) produced by a unit depth of effective rainfall uniformly distributed over the catchment for a specified duration. Once derived, it enables synthesis of storm hydrographs for other runoff depths.
Given Data / Assumptions:
Concept / Approach:
Under linear superposition, a storm DRH equals the UH ordinates scaled by the runoff depth (in the same units as the unit depth defining the UH). If the UH is a 1 cm UH, multiplying factor = runoff depth (mm) / 10; if a 25 mm UH, factor = runoff (mm) / 25. Limited duration mismatch (≈ ±25%) is commonly tolerable, though using a matching-duration UH is best practice.
Step-by-Step Solution:
Transferability: The UH of a given duration can generate future storm hydrographs of like duration → true.Scaling: Multiply UH ordinates by runoff depth in UH-units → true.Factor example: For a 25 mm UH, factor = runoff(mm)/25 → true.Duration tolerance: ±25% is a commonly cited acceptable range → true.
Verification / Alternative check:
Hydrology texts illustrate convolution of a UH with an excess-rain hyetograph to reproduce storm DRHs, confirming the linear scaling of ordinates and practical duration tolerance.
Why Other Options Are Wrong:
Common Pitfalls:
Confusing UH depth (1 cm or 25 mm) with total rainfall depth; or applying UH outside its climatic/catchment context without adjustment.
Final Answer:
All the above.
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