- 2066 Magh (old course) · 16 marks
Construct 3-h UH and flood hydrograph, 524.88 ha
Short answer
Catchment area 524.88 ha yields UH volume 52488 m³; triangular shape with peak at 9 h gives Qp = 1.08 m³/s. 3-h UH ordinates computed. Rainfall excess after φ = 0.333 cm/h: 5, 5, 0, 10 cm in successive 3-h blocks. Superposition with baseflow 20 m³/s gives peak flood 35.7 m³/s at 18 h.
Unit hydrograph of 3h duration from a catchment area of 524.88 ha has peak discharge value after 9 hours from the start of the storm. It has half of the peak discharge value at 3 hours and 15 hours after the start of storm respectively. If time base () is 30 hours, constitute the unit hydrograph and calculate the flood hydrograph from the following rainfall data. Assume the Phi index () as 0.333 cm/hour and base flow as 20 cumecs.
| Time (hours) | 0 | 6 | 9 | 12 |
|---|---|---|---|---|
| Cumulative Rainfall (cm) | 0 | 12 | 12 | 23 |
Step 1: Shape of the 3-h UH
Given: = 30 h, peak at 9 h, half-peak at 3 h and 15 h. So the UH is a straight-line polygon through (0, 0), (3, ½), (9, ), (15, ½) and (30, 0).
Q
Qp | /\
| / \
Qp/2 | / \_
| / \__
0 +--+-----+-----+------+---- t (h)
0 3 9 15 30
Step 2: Peak ordinate from the area
A UH has 1 cm of runoff over the catchment:
Area under the polygon (in units of h):
Step 3: 3-h UH ordinates (3-h interval)
| t (h) | 0 | 3 | 6 | 9 | 12 | 15 | 18 | 21 | 24 | 27 | 30 |
|---|---|---|---|---|---|---|---|---|---|---|---|
| Fraction of Q_p | 0.000 | 0.500 | 0.750 | 1.000 | 0.750 | 0.500 | 0.400 | 0.300 | 0.200 | 0.100 | 0.000 |
| UH (m³/s per cm) | 0.000 | 0.540 | 0.810 | 1.080 | 0.810 | 0.540 | 0.432 | 0.324 | 0.216 | 0.108 | 0.000 |
Step 4: Rainfall excess (3-h blocks)
Cumulative rain: 12 cm at 6 h, still 12 cm at 9 h (no rain 6 – 9 h), 23 cm at 12 h. Rain is taken uniform inside each interval.
| Block | Rain (cm) | Loss φt = 0.333 × 3 (cm) | Excess (cm) |
|---|---|---|---|
| 0 – 3 h | 6 | 1.0 | 5.0 |
| 3 – 6 h | 6 | 1.0 | 5.0 |
| 6 – 9 h | 0 | 0 | 0 |
| 9 – 12 h | 11 | 1.0 | 10.0 |
Step 5: Flood hydrograph
| t (h) | UH (m³/s) | 5 cm × UH | 5 cm × UH | 10 cm × UH | Base | Q (m³/s) |
|---|---|---|---|---|---|---|
| 0 | 0.00 | 0.0 | 0.0 | 0.0 | 20.0 | 20.0 |
| 3 | 0.54 | 2.7 | 0.0 | 0.0 | 20.0 | 22.7 |
| 6 | 0.81 | 4.1 | 2.7 | 0.0 | 20.0 | 26.8 |
| 9 | 1.08 | 5.4 | 4.1 | 0.0 | 20.0 | 29.5 |
| 12 | 0.81 | 4.1 | 5.4 | 5.4 | 20.0 | 34.9 |
| 15 | 0.54 | 2.7 | 4.1 | 8.1 | 20.0 | 34.9 |
| 18 | 0.43 | 2.2 | 2.7 | 10.8 | 20.0 | 35.7 |
| 21 | 0.32 | 1.6 | 2.2 | 8.1 | 20.0 | 31.9 |
| 24 | 0.22 | 1.1 | 1.6 | 5.4 | 20.0 | 28.1 |
| 27 | 0.11 | 0.5 | 1.1 | 4.3 | 20.0 | 25.9 |
| 30 | 0.00 | 0.0 | 0.5 | 3.2 | 20.0 | 23.8 |
| 33 | 0.00 | 0.0 | 0.0 | 2.2 | 20.0 | 22.2 |
| 36 | 0.00 | 0.0 | 0.0 | 1.1 | 20.0 | 21.1 |
| 39 | 0.00 | 0.0 | 0.0 | 0.0 | 20.0 | 20.0 |
Answer: peak flood ≈ 35.66 m³/s at t = 18 h (the flood hydrograph returns to the base flow of 20 m³/s at t = 39 h).
✓ Answer checked by Claude Sonnet 5.5
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