2015
DOI: 10.1016/j.envsoft.2014.10.011
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Modeling surface water-groundwater interaction in arid and semi-arid regions with intensive agriculture

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Cited by 160 publications
(80 citation statements)
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“…Feyen 2005) but not all of them have necessarily been published in peer-reviewed literature. They are often developed by national -Zhangye basin, China, 9,097 km 2 (Tian et al, 2015) (Wilcox et al, 2007) MODCOU / EauDyssée Saleh et al (2011) Pryet et al (2014) ? SAM model (Ledoux et al, 1989;Ledoux et al, 1984) RAPID, 1D Muskingum scheme (David et al, 2011) 1D Stream network hydraulic modelling HEC-RAS (Saleh et al, 2011) Conceptual model soil water-budget (Pryet et al, 2014) -Seine basin, France, 95,600 km 2 (Ledoux et al, 2007) -Rhône basin, 86,500 km 2 (Etchevers et al, 2001) -Upper Rhine basin, 13,900 km 2 (Thierion et al, 2012) -Somme basin, 6,433 km 2 (Habets et al, 2010;Korkmaz et al, 2009) (2000) Kim et al (2008) ?…”
Section: Other Applications Of Loosely Coupled Schemes With Applicatimentioning
confidence: 99%
“…Feyen 2005) but not all of them have necessarily been published in peer-reviewed literature. They are often developed by national -Zhangye basin, China, 9,097 km 2 (Tian et al, 2015) (Wilcox et al, 2007) MODCOU / EauDyssée Saleh et al (2011) Pryet et al (2014) ? SAM model (Ledoux et al, 1989;Ledoux et al, 1984) RAPID, 1D Muskingum scheme (David et al, 2011) 1D Stream network hydraulic modelling HEC-RAS (Saleh et al, 2011) Conceptual model soil water-budget (Pryet et al, 2014) -Seine basin, France, 95,600 km 2 (Ledoux et al, 2007) -Rhône basin, 86,500 km 2 (Etchevers et al, 2001) -Upper Rhine basin, 13,900 km 2 (Thierion et al, 2012) -Somme basin, 6,433 km 2 (Habets et al, 2010;Korkmaz et al, 2009) (2000) Kim et al (2008) ?…”
Section: Other Applications Of Loosely Coupled Schemes With Applicatimentioning
confidence: 99%
“…Then, actual diversion is computed by considering stream routing, and actual pumping is computed by considering the available groundwater in the aquifer. Finally, the actual diversion and pumping is distributed to HRUs by using the method in our previous study [20]. It is noted that the demand for irrigation may not be met 100%, which can be caused by insufficient stream flow or drying of the groundwater wells.…”
Section: Hydrological Modelmentioning
confidence: 99%
“…Tian et al [20] improved the capacity of GSFLOW by adding two new irrigation modules, so it simulates agricultural water management activities. One of the modules is to distribute the diverted water from streams to farmlands through an aqueduct system, and the other is to distribute the abstracted groundwater to the farmlands close to the pumping wells.…”
Section: Hydrological Modelmentioning
confidence: 99%
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“…An improved GSFLOW (Coupled Ground-Water and Surface-Water Flow Model) was used in this study (Tian et al, 2015b), which is capable to explicitly consider irrigation, water diversion and groundwater pumping. GSFLOW integrates a hydrological model PRMS (Precipitation-Runoff Modeling System) and a groundwater model MODFLOW (Modular 5…”
Section: Modelmentioning
confidence: 99%