2020
DOI: 10.1007/s00477-020-01814-z
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Uncertainty of hydrologic simulation, and its impact on the design and the effectiveness of water conservation structures

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Cited by 7 publications
(3 citation statements)
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“…Parameter uncertainties are considered important due to their nature in the hydrological modeling setup and their in uence on the forecasts (Vema et al, 2020). For instance, although the inputs are likely to change according to spatial-temporal coverage, the model parameters are often applied uniformly over the simulation period (Thornton et al, 2021).…”
Section: Parameter Uncertaintymentioning
confidence: 99%
See 1 more Smart Citation
“…Parameter uncertainties are considered important due to their nature in the hydrological modeling setup and their in uence on the forecasts (Vema et al, 2020). For instance, although the inputs are likely to change according to spatial-temporal coverage, the model parameters are often applied uniformly over the simulation period (Thornton et al, 2021).…”
Section: Parameter Uncertaintymentioning
confidence: 99%
“…In this respect, uncertainty in hydrological forecasting may evolve due to one or some of the following reasons: (1) measurement error (Tauro et al, 2018;Vema et al, 2020), (2) input error (Hrachowitz et al, 2013;Tauro et al, 2018;Blöschl et al, 2019), (3) errors in model conceptualization (McInerney et al, 2021), (4) initial setting of the parameters (Vema et al, 2020), (5) simulation error (Tran et al, 2020;Wang et al, 2017, Vema et al, 2020, (6) techniques and assumptions used in calibration procedures (Sivapalan et al, 2003), (7) assumptions used in the hydrological projections (Brigode et al, 2013), and (8) modeler's experience (Moges et al, 2021). Evaluation of recent studies suggests that much progress has been made in addressing the measurements, input, and conceptual uncertainties.…”
Section: Introductionmentioning
confidence: 99%
“…One of the steps in application of these models, is the estimation of their parameters, which is known as model calibration (Guinot et al., 2011; Madsen, 2000; Vema & Sudheer, 2020). Parameters of the hydrological models are estimated by comparing the simulated and observed variables of interest (usually streamflow) (Vema et al., 2020). The match between simulated and observed variables is expressed using statistical performance measures such as Nash Sutcliffe Efficiency (NSE) (Anil et al., 2021; Guo et al., 2018; Nash & Sutcliffe, 1970; Paul et al., 2019; R. Zhang et al., 2018; Tegegne et al., 2017), Kling‐Gupta Efficiency (KGE) (Becker et al., 2019; Brighenti et al., 2019; Garcia et al., 2017; Gupta et al., 2009; Mizukami et al., 2019), Root Mean Squared Error (RMSE) (Kim & Kim, 2020; Y. Zhang et al., 2016) and many others.…”
Section: Introductionmentioning
confidence: 99%