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Flood hydrograph from 6-hr hydrograph, 3.3 and 5.5 cm

Short answer

Separate constant base flow of40 m³/s and derive the6-h UH by dividing DRH by the effective depth 5.021 cm. Convolve the UH with3.3 cm and5.5 cm lagged by6 h, then add base flow. The peak flood is 638 m³/s at 30 h.

Following are the ordinates of hydrograph from a catchment area of 770 km2^2 due to 6-hr rainfall. Derive the ordinates of flood hydrograph due to 3.3 cm and 5.5 cm effective rainfall of duration 6-hr. Make suitable assumptions regarding the base flow.

Time (hr)061218243036424854606672
Discharge (m3^3/s)4065215360400350270205145100705040

Assumption for base flow: the discharge at the start and end of the storm hydrograph is 40 m³/s, so a constant base flow of 40 m³/s is assumed.

Step 1: 6-h UH

Direct runoff ordinates = observed − 40. Volume = (sum of ordinates) × 6 × 3600.

∑DRH=1790 m3/sV=1790×21600=38,664,000 m3depth=VA=38,664,000770×106×100=5.021 cm\begin{aligned} \sum DRH &= 1790 \text{ m}^3/\text{s} \\ V &= 1790\times 21600 = 38,664,000 \text{ m}^3 \\ \text{depth} &= \frac{V}{A} = \frac{38,664,000}{770\times 10^6}\times 100 = 5.021 \text{ cm} \end{aligned}

UH ordinate = DRH / 5.021:

t (h)061218243036424854606672
Observed Q4065215360400350270205145100705040
DRH0251753203603102301651056030100
UH (m³/s per cm)0.05.034.963.771.761.745.832.920.911.96.02.00.0

Step 2: Flood hydrograph

Two successive 6-h effective rains of 3.3 cm and 5.5 cm:

Q(t)=3.3 U(t)+5.5 U(t−6)+40Q(t) = 3.3\,U(t) + 5.5\,U(t-6) + 40
t (h)UH (m³/s)3.3 cm × UH5.5 cm × UHBaseQ (m³/s)
00.000.00.040.040.0
64.9816.40.040.056.4
1234.85115.027.440.0182.4
1863.73210.3191.740.0442.0
2471.69236.6350.540.0627.1
3061.74203.7394.340.0638.1
3645.80151.2339.640.0530.7
4232.86108.4251.940.0400.4
4820.9169.0180.740.0289.7
5411.9539.4115.040.0194.4
605.9719.765.740.0125.4
661.996.632.940.079.4
720.000.011.040.051.0
780.000.00.040.040.0

Answer: peak flood ≈ 638 m³/s at t = 30 h.

✓ Answer checked by Claude Sonnet 5.5

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