This analysis compares various modeling techniques for estimating sediment yield from suspended sediment concentrations, highlighting improved predictions with advanced methods.
For sediment yield estimation, intermittent measurements of suspended sediment concentration (SSC) have to be interpolated toderive a continuous sedigraph. Traditionally, sediment rating curves (SRCs) based on univariate linear regression of dischargeand SSC (or the logarithms thereof) are used but alternative approaches (e.g. fuzzy logic, artificial neural networks, etc.)exist. This paper presents a comparison of the applicability of traditional SRCs, generalized linear models (GLMs) and non-parametric regression using Random Forests (RF) and Quantile Regression Forests (QRF) applied to a dataset of SSC obtainedfor four subcatchments (0Ð08, 41, 145 and 445 km2 ) in the Central Spanish Pyrenees. The observed SSCs are highly variableand range over six orders of magnitude. For these data, traditional SRCs performed inadequately due to the over-simplificationof relating SSC solely to discharge. Instead, the multitude of acting processes required more flexibility to model these nonlinearrelationships. Thus, alternative advanced machine learning techniques that have been successfully applied in other disciplineswere tested. GLMs provide the option of including other relevant process variables (e.g. rainfall intensities and temporalinformation) but require the selection of the most appropriate predictors. For the given datasets, the investigated variableselection methods produced inconsistent results. All proposed GLMs showed an inferior performance, whereas RF and QRFproved to be very robust and performed favourably for reproducing sediment dynamics. QRF additionally provides estimateson the accuracy of the predictions and thus allows the assessment of uncertainties in the estimated sediment yield that is notcommonly found in other methods. The capabilities of RF and QRF concerning the interpretation of predictor effects are alsooutlined
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Francke et al. (2008) studied this question.
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