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...
Main Authors: | , , , |
---|---|
Format: | Article |
Language: | English |
Published: |
MDPI AG
2019-01-01
|
Series: | Water |
Subjects: | |
Online Access: | http://www.mdpi.com/2073-4441/11/1/110 |
id |
doaj-7695db0f0c4d40eab625b06289d6e033 |
---|---|
record_format |
Article |
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 |
work_keys_str_mv |
AT davidchunn applicationofanintegratedswatmodflowmodeltoevaluatepotentialimpactsofclimatechangeandwaterwithdrawalsongroundwatersurfacewaterinteractionsinwestcentralalberta AT monirehfaramarzi applicationofanintegratedswatmodflowmodeltoevaluatepotentialimpactsofclimatechangeandwaterwithdrawalsongroundwatersurfacewaterinteractionsinwestcentralalberta AT briansmerdon applicationofanintegratedswatmodflowmodeltoevaluatepotentialimpactsofclimatechangeandwaterwithdrawalsongroundwatersurfacewaterinteractionsinwestcentralalberta AT danielsalessi applicationofanintegratedswatmodflowmodeltoevaluatepotentialimpactsofclimatechangeandwaterwithdrawalsongroundwatersurfacewaterinteractionsinwestcentralalberta |
_version_ |
1725054147497033728 |