2020
DOI: 10.1002/essoar.10502735.1
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Lake topography and active storage from satellite observations of flood frequency

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Cited by 5 publications
(6 citation statements)
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“…(2006) conducted an extensive bathymetric survey of the Lake Grande do Curuai floodplain, in the eastern Amazon basin. The bathymetry was used to estimate volume, in hydraulic simulation (Rudorff et al., 2014a) and topographic assessment (Fassoni‐Andrade, Paiva, & Fleischmann, 2020). Trigg et al.…”
Section: Surface Watermentioning
confidence: 99%
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“…(2006) conducted an extensive bathymetric survey of the Lake Grande do Curuai floodplain, in the eastern Amazon basin. The bathymetry was used to estimate volume, in hydraulic simulation (Rudorff et al., 2014a) and topographic assessment (Fassoni‐Andrade, Paiva, & Fleischmann, 2020). Trigg et al.…”
Section: Surface Watermentioning
confidence: 99%
“…Furthermore, the proliferation of dams in tropical basins as the Amazon, Congo, and the Mekong require basin‐scale planning and analysis tools to foster mutual benefits in understanding these changes (e.g., Biswas et al., 2021; Latrubesse et al., 2017; Schmitt et al., 2019; Winemiller et al., 2016), and RS data stand out as powerful tool to monitor large scale impacts of existing man‐made reservoirs (e.g., Resende et al., 2019), and infer their characteristics, such as water level and stage‐area‐volume relationships (e.g., Fassoni‐Andrade, Paiva, & Fleischmann, 2020; Gao et al., 2012; Hoek et al., 2019). Better data and knowledge of these impacts are also the base for better hydro‐geomorphological models that could quantify the expected impacts of planned reservoirs and, therefore, aid in creating designs that minimize environmental impacts.…”
Section: Synthesis Of Scientific Advances Future Challenges and Prioritiesmentioning
confidence: 99%
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“…Overall, relative errors are higher upstream, in single channeled, low water height reaches and in the Branco backwater influences. Note that 2D complex lateral flows in floodplains or retention behaviours from "igarape" rivers may happen in high flow periods (see [65,66]).…”
Section: Effective Models Calibration Against Altimetrymentioning
confidence: 99%
“…In addition, HCs were created by identifying the area by water level and the storage capacity using the topographic information of river basins, reservoirs, and wetlands, and the topographic and morphological characteristics of basins were identified and utilized as basic data (Hayashi et al, 2000;Park et al, 2000;Oertel et al, 2000;Kim et al, 2002;6 Kang et al, 2005;Nam et al, 2015). For reservoirs, the morphology index and HC are important information for research on topographic characteristics, and studies that can quantitatively present topographic characteristics are also required (Takeuchi,1997; Leonard et al, 1999;Lehner et al, 2004;Dargahi & Setegn., 2011;Li et al, 2014;Zhang et al, 2017;Lopes et al, 2018;Munar et al, 2018;Andrade et al, 2020).…”
Section: Introductionmentioning
confidence: 99%