Task 1: Associate each hydrological term/method in LIST I with its corresponding purpose or definition in LIST II.
- A. Isohyetal method: This technique calculates the III. Mean areal rainfall for a watershed by constructing contours of equal rainfall depth (isohyets). It is typically the most precise method.
- B. Rational method: An empirical formula (\(Q=CIA\)) used for estimating the I. Peak runoff rate from smaller catchments.
- C. Point rainfall: Rainfall measurement taken at a single location using a II. Reingauge station.
- D. Nash model: This conceptual model represents a watershed as a series of linear reservoirs. It is employed to generate a synthetic unit hydrograph, useful for activities such as IV. Flood routing or runoff prediction from rainfall data.
Task 2: List the correct pairings.
- A \(\rightarrow\) III
- B \(\rightarrow\) I
- C \(\rightarrow\) II
- D \(\rightarrow\) IV
This set of pairings aligns with option (A).