Step 1: Understanding the Concept:
Time of concentration (\(t_c\)) is the time required for storm runoff to travel from the hydraulically most remote point in the watershed to the outlet.
Key Formula or Approach:
\[ t_c = 0.01947 \cdot L^{0.77} \cdot S^{-0.385} \quad \text{(Kirpich's Formula in Metric Units)} \]
where \(t_c\) is in minutes, \(L\) is maximum channel flow length (m), and \(S\) is average channel slope (m/m).
Step 2: Detailed Explanation:
Kirpich (1940) developed an empirical equation based on small agricultural watershed data in Tennessee.
In metric units:
\[ t_c = 0.01947 \times L^{0.77} \times S^{-0.385} \]
It directly computes the Time of Concentration (\(t_c\)) of a watershed from channel length and slope parameters.
Step 3: Final Answer:
Therefore, Kirpich's equation is used to compute Time of concentration, corresponding to option (B).