2017
DOI: 10.1007/s11069-017-2889-0
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Early flood warning in the Itajaí-Açu River basin using numerical weather forecasting and hydrological modeling

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Cited by 35 publications
(10 citation statements)
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“…Also, in the context of operational use, investigations help to highlight the current system problems, whose must be considered when forecast results are to be used for decision making . Some examples of streamflow forecasting studies focusing on its results verifications can be found in recent literature: Bergh and Roulin (2010), Thiemig et al (2010), Schellekens et al (2011), Bao et al (2011), Addor et al (2011), Boucher et al (2011), Bourdin and Stull (2013, Alfieri et al (2014), Pagano (2014), Fan et al ( , 2015a, Siqueira et al (2016a) and Casagrande et al (2017).…”
Section: Introductionmentioning
confidence: 94%
“…Also, in the context of operational use, investigations help to highlight the current system problems, whose must be considered when forecast results are to be used for decision making . Some examples of streamflow forecasting studies focusing on its results verifications can be found in recent literature: Bergh and Roulin (2010), Thiemig et al (2010), Schellekens et al (2011), Bao et al (2011), Addor et al (2011), Boucher et al (2011), Bourdin and Stull (2013, Alfieri et al (2014), Pagano (2014), Fan et al ( , 2015a, Siqueira et al (2016a) and Casagrande et al (2017).…”
Section: Introductionmentioning
confidence: 94%
“…In this paper, the probabilistic streamflow forecasts were generated using ensemble weather forecasts from two The MHD-INPE hydrological model is a regular grid-based model that uses a combination of the Xinanjiang model probabilistic approach and the TopModel formulation to simulate runoff generation. This model has been used in climate change studies (Mohor, Rodriguez, Tomasella, & Siqueira Júnior, 2015;Siqueira-Jr et al, 2015), land use and land cover change studies and for flood forecasting studies (Casagrande et al, 2017;Falck, Maggioni, Tomasella, Vila, & Diniz, 2015). For a detailed description of the MHD-INPE model, the reader is referred to Rodriguez and Tomasella (2015).…”
Section: Numerical Modelsmentioning
confidence: 99%
“…Fan, Schwanenberg, Collischonn, and Weerts (); Fan et al (, ) assessed the performances of three‐month seasonal forecasts in the upper São Francisco, Tocantins and Doce River basins in terms of their ability to predict reservoir inflow for management purposes using different EPS numerical models. In terms of short‐term flood forecasts, Siqueira, Collischonn, Fan, and Chou () and Casagrande, Tomasella, dos Santos Alvalá, Bottino, and Caram () tested the feasibility of the regional Eta model EPS in the Taquari Antas and Itajaí‐Açu basins, respectively, and concluded that the flood forecasts can be improved by using the EPS technique, mainly in terms of the lead time.…”
Section: Introductionmentioning
confidence: 99%
“…Increasing interaction and exposure between human systems and river floodplains, as well as uncertainties in the context of a changing climate (Di Baldassarre et al 2013Baldassarre et al , 2018Hirabayashi et al 2013;Blöschl et al 2015;Winsemius et al 2016), highlight the importance of improving our capability to evaluate flood control measures and understand the associated changes on variables as water level, discharge, floodplain storage and water velocity. Large-scale hydrologic models are powerful tools for flood-related studies such as prediction of future flood risk under climate change (Hirabayashi et al 2013;Winsemius et al 2016;Ribeiro Neto et al 2016), flood hazard mapping (Pappenberger et al 2012) and flood forecasting (Alfieri et al 2013;Paiva et al 2013;Fan et al 2016;Siqueira et al 2016a;Casagrande et al 2017). Recent years have seen a major development of coupling strategies between hydrologic and 1D and 2D hydrodynamic models (Biancamaria et al 2009;Yamazaki et al 2011;Neal et al 2012;Paiva et al 2013;Schumann et al 2013;Seibert et al 2014;Hoch et al 2017a;Pontes et al 2017;Fleischmann et al 2018), which relevance was generally justified by a misrepresentation of flood dynamics in simpler models (e.g., flood peak attenuation due to floodplains, flood wave diffusion).…”
Section: Introductionmentioning
confidence: 99%