Universiti Teknologi Malaysia Institutional Repository

A calibrated, watershed-specific SCS-CN method: Application to Wangjiaqiao watershed in the three gorges area, China

Ling, Lloyd and Yusop, Zulkifli and Yap, Wun She and Tan, Wei Lun and Chow, Ming Fai and Ling, Joan Lucille (2020) A calibrated, watershed-specific SCS-CN method: Application to Wangjiaqiao watershed in the three gorges area, China. Water (Switzerland), 12 (1). p. 60. ISSN 2073-4441

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Official URL: http://dx.doi.org/10.3390/w12010060

Abstract

The Soil Conservation Service curve number (SCS-CN) method is one of the most popular methods used to compute runoff amount due to its few input parameters. However, recent studies challenged the inconsistent runoff results obtained by the method which set the initial abstraction ratio λ as 0.20. This paper developed a watershed-specific SCS-CN calibration method using non-parametric inferential statistics with rainfall-runoff data pairs. The proposed method first analyzed the data and generated confidence intervals to determine the optimum values for SCS-CN model calibration. Subsequently, the runoff depth and curve number were calculated. The proposed method outperformed the runoff prediction accuracy of the asymptotic curve number fitting method, linear regression model and the conventional SCS-CN model with the highest Nash-Sutcliffe index value of 0.825, the lowest residual sum of squares value of 133.04 and the lowest prediction error. It reduced the residual sum of squares by 66% and the model prediction errors by 96% when compared to the conventional SCS-CN model. The estimated curve number was 72.28, with the confidence interval ranging from 62.06 to 78.00 at a 0.01 confidence interval level for the Wangjiaqiao watershed in China.

Item Type:Article
Uncontrolled Keywords:Bootstrap, Curve number
Subjects:T Technology > TA Engineering (General). Civil engineering (General)
Divisions:Civil Engineering
ID Code:91220
Deposited By: Widya Wahid
Deposited On:21 Jun 2021 08:41
Last Modified:21 Jun 2021 08:41

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