Abstract

Abstract. In many situations the extension of hydrological or water quality time series at short-gauged stations is required. Ordinary least squares regression (OLS) of any hydrological or water quality variable is a traditional and commonly used record extension technique. However, OLS tends to underestimate the variance in the extended records, which leads to underestimation of high percentiles and overestimation of low percentiles, given that the data are normally distributed. The development of the line of organic correlation (LOC) technique is aimed at correcting this bias. On the other hand, the Kendall-Theil robust line (KTRL) method has been proposed as an analogue of OLS with the advantage of being robust in the presence of outliers. Given that water quality data are characterised by the presence of outliers, positive skewness and non-normal distribution of data, a robust record extension technique is more appropriate. In this paper, four record-extension techniques are described, and their properties are explored. These techniques are OLS, LOC, KTRL and a new technique proposed in this paper, the robust line of organic correlation technique (RLOC). RLOC includes the advantage of the LOC in reducing the bias in estimating the variance, but at the same time it is also robust in the presence of outliers. A Monte Carlo study and empirical experiment were conducted to examine the four techniques for the accuracy and precision of the estimate of statistical moments and over the full range of percentiles. Results of the Monte Carlo study showed that the OLS and KTRL techniques have serious deficiencies as record-extension techniques, while the LOC and RLOC techniques are nearly similar. However, RLOC outperforms OLS, KTRL and LOC when using real water quality records.

Highlights

  • In many cases, water resources management involves the use of different hydrologic or water quality data to simulate the outcomes of decisions (Hirsch, 1982)

  • The ordinary least squares regression (OLS), Kendall-Theil robust line (KTRL), line of organic correlation (LOC) and the new robust line of organic correlation (RLOC) technique were compared in this study using a Monte Carlo and empirical experiments using water quality data from the Edko drainage system, in the Nile Delta of Egypt

  • In the assessment of the errors of the extended records using BIAS and root mean squared error (RMSE), the Monte Carlo experiment revealed that when OLS assumptions are fulfilled, it outperforms the other three techniques

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Summary

Introduction

Water resources management involves the use of different hydrologic or water quality data to simulate the outcomes of decisions (Hirsch, 1982). Records available for many streams are either too short to contain a sufficient range of hydrologic and water quality conditions or have periods of missing data (Alley and Burns, 1983) One solution to this problem is to rely on the transfer of information from nearby stream gauges with available longterm records (Hirsch, 1982; Alley and Burns, 1983; Vogel and Stedinger, 1985). This can be done by extending historic hydrologic or water quality records of interest in time via extrapolation of the correlation between these records at the site of interest and concurrent records at a nearby site. OLS is commonly applied to reconstitute information about short-gauged water quality variables (Harmancioglu and Yevjevich, 1986, 1987; Harmancioglu et al, 1999; Robinson et al, 2004; Khalil and Ouarda, 2009)

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