2016
DOI: 10.1016/j.jhydrol.2015.11.025
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A MODFLOW package to linearize stream depletion analysis

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Cited by 6 publications
(5 citation statements)
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“…The SWAT-MODFLOW coupled model takes advantage of the respective strengths of the above two models by feeding an input of HRU-based groundwater recharge calculated by the SWAT model to the MODFLOW model, and MODFLOW calculates the groundwater flow between the aquifer and the river channel and returns it back to SWAT [31,32]. In this way, the spatiotemporal characteristics of the groundwater-dominated watersheds can be reasonably displayed, and the water cycle processes can be more accurately modelled.…”
Section: The Swat-modflow Modelmentioning
confidence: 99%
“…The SWAT-MODFLOW coupled model takes advantage of the respective strengths of the above two models by feeding an input of HRU-based groundwater recharge calculated by the SWAT model to the MODFLOW model, and MODFLOW calculates the groundwater flow between the aquifer and the river channel and returns it back to SWAT [31,32]. In this way, the spatiotemporal characteristics of the groundwater-dominated watersheds can be reasonably displayed, and the water cycle processes can be more accurately modelled.…”
Section: The Swat-modflow Modelmentioning
confidence: 99%
“…When considered individually or used to generate maps or rankings, we refer to them by the more intuitive term "depletion potential." Depletion potential (e.g., Ahlfeld et al 2016) can be calculated in a variety of ways including using Adjoint State (Neupauer and Griebling 2012;Griebling and Neupauer 2013) and reformulation of the underlying process model (Ou et al 2016).…”
Section: Depletion Potentialmentioning
confidence: 99%
“…One notable example is MODFLOW, a 3D finite difference model designed specifically for simulating groundwater flows [6,7]. MODFLOW has been extensively used by researchers to simulate groundwater levels across diverse regions (Dong et al, 2012;Lachaal et al, 2012;Ou et al, 2013Ou et al, , 2016Chen et al, 2017). For instance, Coelho et al (2017) utilized field data from an aquifer in a watershed in Vicosa, Minas Gerais, Brazil to assess different numerical hydrological models under varying boundary conditions.…”
Section: Introductionmentioning
confidence: 99%