Difficulty: Easy
Correct Answer: Rainfall characteristics and drainage area
Explanation:
Introduction / Context:
Regional empirical relations for design discharge often appear in the form of unit discharge (cumecs per km^2). The Boston Society of Civil Engineers (B.S.C.E.) relation is a classical example linking peak runoff to catchment size and rainfall. Recognizing the governing variables helps engineers apply such formulae appropriately and understand their limitations.
Given Data / Assumptions:
Concept / Approach:
Unit discharge normalizes by area, so remaining primary drivers are rainfall (intensity/duration appropriate to the basin response) and catchment properties. In these simplified relations, area is always present; rainfall is the forcing input. Basin shape or total runoff volume are not typically the core variables in the simple B.S.C.E. peak relation stated per unit area.
Step-by-Step Reasoning:
Identify required variables for peak runoff generation: rainfall forcing + catchment size.Other details (shape, slope, infiltration) are often embedded in empirical coefficients; they are not the explicit paired factors in the simplest expression.
Verification / Alternative check:
Many historical US and regional formulae express Q = C * P^m * A^n; when cast per unit area, Q/A primarily scales with P and weakly with A through the exponent or coefficient. This supports option (a).
Why Other Options Are Wrong:
Common Pitfalls:
Final Answer:
Rainfall characteristics and drainage area
Discussion & Comments