Step 1: Match each hydrological term/method in LIST I with its purpose or definition in LIST II.
- A. Isohyetal method: This is a technique for calculating the III. Mean areal rainfall over a watershed by drawing contours of equal rainfall depth (isohyets). It is generally the most accurate method.
- B. Rational method: A simple empirical formula (\(Q=CIA\)) used to estimate the I. Peak runoff rate from small catchments.
- C. Point rainfall: This is the rainfall measured at a single location by a II. Reingauge station.
- D. Nash model: The Nash model conceptualizes a watershed as a cascade of linear reservoirs. It is a conceptual model used to derive a synthetic unit hydrograph, which is then used for tasks like IV. Flood routing or predicting runoff from rainfall.
Step 2: Compile the correct pairings.
- A \(\rightarrow\) III
- B \(\rightarrow\) I
- C \(\rightarrow\) II
- D \(\rightarrow\) IV
This combination corresponds to option (A).