2019
DOI: 10.1016/j.jhydrol.2019.123957
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Hydrological post-processing using stacked generalization of quantile regression algorithms: Large-scale application over CONUS

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Cited by 72 publications
(70 citation statements)
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“…Under the stationarity and ergodicity assumptions (see e.g., Koutsoyiannis and Montanari 2015 for the implications of these assumptions in hydrological contexts), the trained error model can then be applied in the period T3 for converting a point hydrological prediction obtained using the same hydrological model with the same parameters into a probabilistic hydrological prediction. The error model could fall into the category of conditional distribution models (see e.g., Montanari and Brath 2004;Montanari and Grossi 2008) or the category of statistical learning regression models that can directly provide predictive quantiles instead of predictive PDFs (see e.g., Dogulu et al 2015;López López et al 2014;Papacharalampous et al 2019b;Tyralis et al 2019b), amongst other model categories.…”
Section: Methodological Background On Two-stage Post-processingmentioning
confidence: 99%
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“…Under the stationarity and ergodicity assumptions (see e.g., Koutsoyiannis and Montanari 2015 for the implications of these assumptions in hydrological contexts), the trained error model can then be applied in the period T3 for converting a point hydrological prediction obtained using the same hydrological model with the same parameters into a probabilistic hydrological prediction. The error model could fall into the category of conditional distribution models (see e.g., Montanari and Brath 2004;Montanari and Grossi 2008) or the category of statistical learning regression models that can directly provide predictive quantiles instead of predictive PDFs (see e.g., Dogulu et al 2015;López López et al 2014;Papacharalampous et al 2019b;Tyralis et al 2019b), amongst other model categories.…”
Section: Methodological Background On Two-stage Post-processingmentioning
confidence: 99%
“…Here the interest is on probabilistic hydrological post-processing methodologies, in which the error model is estimated conditional upon the point prediction(s) of the hydrological model by using an independent segment (with respect to the one used for estimating the parameters of the hydrological model) extracted from the historical dataset. Various methodologies of this category are currently available (see e.g., Bock et al 2018;Bourgin et al 2015;Dogulu et al 2015;Farmer and Vogel 2016;López López et al 2014;Montanari and Brath 2004;Montanari and Grossi 2008;Montanari and Koutsoyiannis 2012;Solomatine and Shrestha 2009;Papacharalampous et al 2019b;Tyralis et al 2019b;Wani et al 2017), amongst other probabilistic hydrological modelling and hydrological forecasting methodologies based on the idea of integrating process-based models and statistical approaches (see e.g., Beven and Binley 1992; Hernández- López and Francés 2017;Kavetski et al 2002;2006, Krzysztofowicz 1999, 2001, 2002Kelly 2000, Krzysztofowicz andHerr 2001;Todini 2008; see also the review of Montanari 2011). Hereafter, we use the comprehensive term "two-stage" by Evin et al (2014) to imply that the parameters of a probabilistic hydrological post-processing methodology are estimated within two subsequent stages.…”
Section: Introductionmentioning
confidence: 99%
“…The quantile regression model is a balanced choice between interpretable and more flexible algorithms from the statistical learning literature. It has already been applied for post-processing hydrological predictions within hydrological modelling case studies (see e.g., Dogulu et al 2015, López López et al 2014, Solomatine and Shrestha 2009, Wani et al 2017, while its use is more common in the field of hydrological forecasting (see e.g., Tyralis et al 2019a and the references therein); see also the references in Dogulu et al (2015) for applications of this model in other geoscience concepts.…”
Section: Introductionmentioning
confidence: 99%
“…For benchmarking purposes, we also apply the working methodology using the linear regression model (see e.g., James et al 2013;Hastie et al 2009) as error model, and the two naïve probabilistic data-driven schemes. For the merits of using benchmarks in hydrological modelling, the reader is referred to Pappenberger et al (2015); see also benchmarking examples in Montanari and Brath (2004), Papacharalampous and Tyralis (2018), Papacharalampous et al (2018aPapacharalampous et al ( ,b,c, 2019a, Quilty et al (2019), Evin et al (2014), Sikorska et al (2015), Papacharalampous (2017, 2018), Tyralis et al ( , 2019a, and Xu et al (2018).…”
Section: Introductionmentioning
confidence: 99%
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