Application of an Integrated SWAT–MODFLOW Model to Evaluate Potential Impacts of Climate Change and Water Withdrawals on Groundwater–Surface Water Interactions in West-Central Alberta

It has become imperative that surface and groundwater resources be managed as a holistic system. This study applies a coupled groundwater–surface water (GW–SW) model, SWAT–MODFLOW, to study the hydrogeological conditions and the potential impacts of climate change and g...

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Main Authors: David Chunn, Monireh Faramarzi, Brian Smerdon, Daniel S. Alessi
Format: Article
Language:English
Published: MDPI AG 2019-01-01
Series:Water
Subjects:
Online Access:http://www.mdpi.com/2073-4441/11/1/110
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spelling doaj-7695db0f0c4d40eab625b06289d6e0332020-11-25T01:38:23ZengMDPI AGWater2073-44412019-01-0111111010.3390/w11010110w11010110Application of an Integrated SWAT–MODFLOW Model to Evaluate Potential Impacts of Climate Change and Water Withdrawals on Groundwater–Surface Water Interactions in West-Central AlbertaDavid Chunn0Monireh Faramarzi1Brian Smerdon2Daniel S. Alessi3Department of Earth and Atmospheric Sciences, University of Alberta, Edmonton, AB, T6G 2E3, CanadaDepartment of Earth and Atmospheric Sciences, University of Alberta, Edmonton, AB, T6G 2E3, CanadaAlberta Geological Survey, Alberta Energy Regulator, Edmonton, AB, T6B 2X3, CanadaDepartment of Earth and Atmospheric Sciences, University of Alberta, Edmonton, AB, T6G 2E3, CanadaIt has become imperative that surface and groundwater resources be managed as a holistic system. This study applies a coupled groundwater–surface water (GW–SW) model, SWAT–MODFLOW, to study the hydrogeological conditions and the potential impacts of climate change and groundwater withdrawals on GW–SW interactions at a regional scale in western Canada. Model components were calibrated and validated using monthly river flow and hydraulic head data for the 1986–2007 period. Downscaled climate projections from five General Circulation Models (GCMs), under the RCP 8.5, for the 2010–2034 period, were incorporated into the calibrated model. The results demonstrated that GW–SW exchange in the upstream areas had the most pronounced fluctuation between the wet and dry months under historical conditions. While climate change was revealed to have a negligible impact in the GW–SW exchange pattern for the 2010–2034 period, the addition of pumping 21 wells at a rate of 4680 m3/d per well to support hypothetical high-volume water use by the energy sector significantly impacted the exchange pattern. The results showed that the total average discharge into the rivers was only slightly reduced from 1294 m3/d to 1174 m3/d; however, localized flowrate differences varied from under 5 m3/d to over 3000 m3/d in 320 of the 405 river cells. The combined potential impact is that intensive groundwater use may have more immediate effects on river flow than those of climate change, which has important implications for water resources management and for energy supply in the future.http://www.mdpi.com/2073-4441/11/1/110hydrogeologymodellingcalibrationuncertainty analysisgroundwater pumpingwater resources management
collection DOAJ
language English
format Article
sources DOAJ
author David Chunn
Monireh Faramarzi
Brian Smerdon
Daniel S. Alessi
spellingShingle David Chunn
Monireh Faramarzi
Brian Smerdon
Daniel S. Alessi
Application of an Integrated SWAT–MODFLOW Model to Evaluate Potential Impacts of Climate Change and Water Withdrawals on Groundwater–Surface Water Interactions in West-Central Alberta
Water
hydrogeology
modelling
calibration
uncertainty analysis
groundwater pumping
water resources management
author_facet David Chunn
Monireh Faramarzi
Brian Smerdon
Daniel S. Alessi
author_sort David Chunn
title Application of an Integrated SWAT–MODFLOW Model to Evaluate Potential Impacts of Climate Change and Water Withdrawals on Groundwater–Surface Water Interactions in West-Central Alberta
title_short Application of an Integrated SWAT–MODFLOW Model to Evaluate Potential Impacts of Climate Change and Water Withdrawals on Groundwater–Surface Water Interactions in West-Central Alberta
title_full Application of an Integrated SWAT–MODFLOW Model to Evaluate Potential Impacts of Climate Change and Water Withdrawals on Groundwater–Surface Water Interactions in West-Central Alberta
title_fullStr Application of an Integrated SWAT–MODFLOW Model to Evaluate Potential Impacts of Climate Change and Water Withdrawals on Groundwater–Surface Water Interactions in West-Central Alberta
title_full_unstemmed Application of an Integrated SWAT–MODFLOW Model to Evaluate Potential Impacts of Climate Change and Water Withdrawals on Groundwater–Surface Water Interactions in West-Central Alberta
title_sort application of an integrated swat–modflow model to evaluate potential impacts of climate change and water withdrawals on groundwater–surface water interactions in west-central alberta
publisher MDPI AG
series Water
issn 2073-4441
publishDate 2019-01-01
description It has become imperative that surface and groundwater resources be managed as a holistic system. This study applies a coupled groundwater–surface water (GW–SW) model, SWAT–MODFLOW, to study the hydrogeological conditions and the potential impacts of climate change and groundwater withdrawals on GW–SW interactions at a regional scale in western Canada. Model components were calibrated and validated using monthly river flow and hydraulic head data for the 1986–2007 period. Downscaled climate projections from five General Circulation Models (GCMs), under the RCP 8.5, for the 2010–2034 period, were incorporated into the calibrated model. The results demonstrated that GW–SW exchange in the upstream areas had the most pronounced fluctuation between the wet and dry months under historical conditions. While climate change was revealed to have a negligible impact in the GW–SW exchange pattern for the 2010–2034 period, the addition of pumping 21 wells at a rate of 4680 m3/d per well to support hypothetical high-volume water use by the energy sector significantly impacted the exchange pattern. The results showed that the total average discharge into the rivers was only slightly reduced from 1294 m3/d to 1174 m3/d; however, localized flowrate differences varied from under 5 m3/d to over 3000 m3/d in 320 of the 405 river cells. The combined potential impact is that intensive groundwater use may have more immediate effects on river flow than those of climate change, which has important implications for water resources management and for energy supply in the future.
topic hydrogeology
modelling
calibration
uncertainty analysis
groundwater pumping
water resources management
url http://www.mdpi.com/2073-4441/11/1/110
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