Probabilistic properties of the Curve Number Agnieszka Rutkowska 1) , Kazimierz Banasik 2) , Silvia Kohnova 3) , Beata Karabova 3) European Geosciences Union General Assembly, Vienna, 07-12 April 2013 1) Department of Applied Mathematics, University of Agriculture in Krakow, Poland 2) Department of Water Engineering, Warsaw University of Life Sciences - SGGW, Poland 3) Department of Land and Water Resources Management, Slovak University of Technology in Bratislava, Slovakia 1 The main problem What is the variability of the Curve Number in the SCS-CN method? 2 Abstract The SCS-CN method allows to predict the runoff volume in small, ungauged catchments. Due to observed variability of the CN, its probabilistic properties in Slovakian and Polish catchments were analyzed. Results contain: the determination of the theoretical distribution function, confidence intervals, comparison to ARC I and ARC III and the asymptotic fitting. 3 Catchments A. The Zago ˙ z z onka River, centre of Poland B. Carpathian Slovakian catchments: Stupavsk´ y, Raˇ ciansk´ y, Gidra, Viˇ stuk, Petrinovec, C. Carpathian Polish catchments: Poniczanka, Mszanka, Kasinianka, Lubie´ nka, Skawica. 4 The SCS-CN method The SCS-CN equations: H = (P λS ) 2 P +(1λ)S if P λS , 0 otherwise and S = 254( 100 CN 1) H the direct runoff, P the rainfall depth, S the watershed storage parameter λthe initial abstraction ratio. CN depends on land use and soil type, in the model is assumed to be constant and is tabulated CN theor In practiceCN varies and is a random variable 5 Sample analysis The solution of the SCS-CN equations if λ =0.2 is CN = 25400 S +254 where S = 5(P +2H 4H 2 +5PH ) For events (P i , H i ) we get a sample CN i . The empirical density function of the CN is negatively skewed The variable 100 CN is positively skewed. It was investigated to fit a typical theoretical distribution function [3]. 6 Distribution fitting Statistical tests of goodness of fit: Kolmogorov-Smirnov (KS), Cramer-von Mises (CM), Anderson-Darling, Shapiro-Wilk. Quantile-Quantile plots and correlation coeff. r . Criteria: (a) W = KS + CM +1 r 2 achieves minimum (b) Akaike Information Criterion (AIC) Theoretical distribution for 100 CN is Generalized Extreme Value. 7 Confidence intervals and ARC I, III Confidence intervals indicate the most probable CN s. The comparison to the CN (I ) and CN (III ) conditions (Hawkins formula) implies the SCS-CN model may overestimate the direct runoff (Stupavsk´ y, Raˇ ciansk´ y) underestimate the direct runoff (Petrinovec, Poniczanka, Skawica). 8 The asymptotic fitting The drift of CN s with increasing rainfall depth [2] is recognized using lim P →∞ CN (P , H ) where P , H are independently sorted P and H . Stupavsk´ y: CN (P ) = 41.23 + 58, 77e 0.02P Petrinovec: CN (P ) = 63.53 + 36.47e 0.03P Zago ˙ z z onka (result of Banasik, Woodward [1]): CN (P ) = 74.03 + 25.97e 0.06P 9 Acknowledgments The investigation described in the contribution has been initiated by first Author research visit to Technical University of Bratislava in 2012 within a STSM of the COST Action ES0901. Polish data used here have been provided by research project no. N N305 396238 founded by PL-Ministry of Science and Higher Education. This work was also supported by the Slovak Research and Development Agency under the contract No. APVV-0015-10 and APVV-0496-10. The support provided by the organizations is gratefully acknowledged. 10 References [1] Banasik K., Woodward D. (2010) Empirical determination of runoff Curve Number for a small agricultural watershed in Poland 2nd Joint Federal Interagency Conference, Las Vegas, NV, June 27 - July 1. [2] Hawkins RH. (1993) Asymptotic determination of curve numbers from data Journal of Irrigation and Drainage Division, American Society of Civil Engineers, 119(2), p. 334-345. [3] McCuen R. (2002) Approach to Confidence Interval Estimation for Curve Numbers Journal of Hydrologic Engineering, 7, p. 43-48, DOI: 10.1061/(ASCE)1084-0699(2002)7:1(43).