The SCS curve number (CN) is a method developed by the USDA in 1995, when is was formerly named Soil Conservation Service, hence the SCS in the name. 1 CN helps with the estimation of runoff at basins where no runoff has been measured. The CN (curve number) ranges from 0 to 100 and is a dimensionless index representing the combined effect of LU/LC, Soil type and hydrological conditions. CN is used to calculate the potential maximum retention capacity \(S\)
\[
S = \dfrac{25400}{CN}-254
\] where the CN = 0 means complete infiltration, CN = 100 no infiltration at all.
The method estimates the precipitation excess \(P_e\) as a function of the cumulative precipitation depth, soil cover, land use, and antecedent soil moisture as
\[
P_e = \begin{cases}
0, \text{ for }\qquad P < I_a\\
\dfrac{(P-I_a)^2}{P - I_a + S}\qquad \text{otherwise }
\end{cases}
\]
where \(P_e\) is accumulated precipitation excess. \(P\) is the accummulated precipitation depth, \(I_a\) is the initial abstraction (loss) and \(S\) is the potential maximum retention
We have to start with some initial data.
\[
\dfrac{F}{S} = \dfrac{Q}{P-I_a}
\]
\[
I_a = rS\approx0.2\cdot S
\]
\[
S = \dfrac{1000}{\mathrm{CN}}-10\:\mathrm{[mm]}
\] where \(S\) is a potential maximum retention after the initial runoff.
# Function to calculate direct runoff using SCS CN methodscs_cn_method <-function(P, CN) { S <- (25400/ CN) -254 Ia <-0.1* Sifelse(P <= Ia, 0, ((P - Ia)^2) / (P - Ia + S))}
1
Maximum potential retention (mm)
3
Calculate runoff
Code
precipitation <-seq(0, 200, by =1)curve_numbers <-seq(from =40, to =100, by =5)# Calculate runoff for each CNrunoff_results <-sapply(curve_numbers, function(CN) {sapply(precipitation, scs_cn_method, CN = CN)})# Plot resultsplot(NULL, xlim =c(0, max(precipitation)), ylim =c(0, max(runoff_results)),xlab ="Precipitation (mm)", ylab ="Runoff (mm)", main ="SCS Curve Number Method: Runoff vs. Precipitation")for (i inseq_along(curve_numbers)) {lines(precipitation, runoff_results[, i], col ="black", lty = i, lwd =1)}# Add legendlegend("topright", legend =paste("CN =", curve_numbers), col ="black", lty = i, lwd =1)
# Example measured precipitation time series (daily data in mm)precipitation <- dat01138000$prec[100:1000]# Define Curve NumberCN <-75# Example value for a watershed# Calculate runoff for each dayrunoff <-sapply(precipitation, scs_cn_method, CN = CN)# Create a time vector for plottingdays <-seq_along(precipitation)# Plot precipitation and runoffplot(days, precipitation, type ="h", col ="black", lwd =0.5, ylim =c(0, max(c(precipitation, runoff), na.rm =TRUE)),xlab ="Day", ylab ="Value (mm)", main ="CN based Precipitation and Runoff", lty =3)lines(x = days, y = runoff, type ="h", col ="#0088BB", lty =1, lwd =1.5)legend("topright", legend =c("Precipitation", "Runoff"), col =c("black", "#0088BB"), lty =c(3, 1), lwd =c(0.5, 1.5))
Exercise
In practice we would have more than one CN type in the watershed. Estimate the runoff from the watershed using the SCS CN method. Using the following data.
HRU
Area
CN\(_i\)
1
20
70
2
16
84
3
64
74
Compare two approaches to calculate runoff.
Weighted average of CN curves
Weighted contribution to discharge (separate contribution, first compute runoff and weight apply weights by fraction of area).