2018
DOI: 10.5194/gmd-11-4755-2018
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GSFLOW–GRASS v1.0.0: GIS-enabled hydrologic modeling of coupled groundwater–surface-water systems

Abstract: Abstract. The importance of water moving between the atmosphere and aquifers has led to efforts to develop and maintain coupled models of surface water and groundwater. However, developing inputs to these models is usually time-consuming and requires extensive knowledge of software engineering, often prohibiting their use by many researchers and water managers, thus reducing these models' potential to promote science-driven decision-making in an era of global change and increasing water resource stress. In res… Show more

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Cited by 20 publications
(21 citation statements)
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“…Flow-routing algorithms are applied across a broad range of fields, including hydrologic and geomorphic modelling, topographic analysis, planetary science, and palaeoclimate. They are a critical component of both hydrologic (Neal et al, 2011;Ng et al, 2018;Ray et al, 2016) and geomorphic (Adams et al, 2017;Coulthard et al, 2013) models, with the former including watershed-scale processes and flood risk. In the latter case, flow routing is often recomputed over time to simulate the feedback between evolving topography and drainage patterns (Hobley et al, 2017;Tucker et al, 2011).…”
Section: Introductionmentioning
confidence: 99%
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“…Flow-routing algorithms are applied across a broad range of fields, including hydrologic and geomorphic modelling, topographic analysis, planetary science, and palaeoclimate. They are a critical component of both hydrologic (Neal et al, 2011;Ng et al, 2018;Ray et al, 2016) and geomorphic (Adams et al, 2017;Coulthard et al, 2013) models, with the former including watershed-scale processes and flood risk. In the latter case, flow routing is often recomputed over time to simulate the feedback between evolving topography and drainage patterns (Hobley et al, 2017;Tucker et al, 2011).…”
Section: Introductionmentioning
confidence: 99%
“…In the latter case, flow routing is often recomputed over time to simulate the feedback between evolving topography and drainage patterns (Hobley et al, 2017;Tucker et al, 2011). Flow-routing calculations and drainage network construction also form the basis for topographic analysis algorithms to automatically pick channel heads (Clubb et al, 2014;Passalacqua et al, 2010;Pelletier, 2013), segment watersheds into representative hydrological units (Czuba and Foufoula-Georgiou, 2014;Ng et al, 2018;Teng et al, 2017), and link river-channel form with rates of tectonic uplift (Duvall et al, 2004;Perron and Royden, 2013;Willgoose et al, 1991) or subsidence (Paola et al, 1992;Wickert and Schildgen, 2019). These same tools have been applied to understand valley networks on Mars (Luo and Stepinski, 2009;Molloy and Stepinski, 2007), the impacts of freshwater forcing on climate during the most recent deglaciation (Ivanovic et al, 2017(Ivanovic et al, , 2018Riddick et al, 2018), and links between palaeo-drainage networks and modern economic and agri-cultural resources (Craddock et al, 2010).…”
Section: Introductionmentioning
confidence: 99%
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“…Сучасні дослідження та розвиток ГІС інструментарію для розв'язання гідрологічних задач можна побачити в роботах [7][8][9][10][11][12][13][14][15][16][17].…”
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