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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 (tbt_b) is 30 hours, constitute the unit hydrograph and calculate the flood hydrograph from the following rainfall data. Assume the Phi index (ϕ\phi) as 0.333 cm/hour and base flow as 20 cumecs.

Time (hours)06912
Cumulative Rainfall (cm)0121223

Step 1: Shape of the 3-h UH

Given: tbt_b = 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, ½QpQ_p), (9, QpQ_p), (15, ½QpQ_p) 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:

V=524.88 ha×104×0.01 m=52 488 m3V = 524.88\text{ ha}\times 10^4 \times 0.01 \text{ m} = 52\,488 \text{ m}^3

Area under the polygon (in units of Qp⋅Q_p\cdoth):

12(3)(0.5)+12(0.5+1)(6)+12(1+0.5)(6)+12(15)(0.5)=0.75+4.5+4.5+3.75=13.5\tfrac12(3)(0.5) + \tfrac12(0.5+1)(6) + \tfrac12(1+0.5)(6) + \tfrac12(15)(0.5) = 0.75+4.5+4.5+3.75 = 13.5 Qp×13.5×3600=52 488 ⇒ Qp=1.08 m3/sQ_p \times 13.5 \times 3600 = 52\,488 \ \Rightarrow\ Q_p = 1.08 \text{ m}^3/\text{s}

Step 3: 3-h UH ordinates (3-h interval)

t (h)036912151821242730
Fraction of Q_p0.0000.5000.7501.0000.7500.5000.4000.3000.2000.1000.000
UH (m³/s per cm)0.0000.5400.8101.0800.8100.5400.4320.3240.2160.1080.000

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.

BlockRain (cm)Loss φt = 0.333 × 3 (cm)Excess (cm)
0 – 3 h61.05.0
3 – 6 h61.05.0
6 – 9 h000
9 – 12 h111.010.0

Step 5: Flood hydrograph

Q(t)=5 U(t)+5 U(t−3)+0⋅U(t−6)+10 U(t−9)+20Q(t) = 5\,U(t) + 5\,U(t-3) + 0\cdot U(t-6) + 10\,U(t-9) + 20
t (h)UH (m³/s)5 cm × UH5 cm × UH10 cm × UHBaseQ (m³/s)
00.000.00.00.020.020.0
30.542.70.00.020.022.7
60.814.12.70.020.026.8
91.085.44.10.020.029.5
120.814.15.45.420.034.9
150.542.74.18.120.034.9
180.432.22.710.820.035.7
210.321.62.28.120.031.9
240.221.11.65.420.028.1
270.110.51.14.320.025.9
300.000.00.53.220.023.8
330.000.00.02.220.022.2
360.000.00.01.120.021.1
390.000.00.00.020.020.0

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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