Potential Hydrologic Impact of Climate Change to Athabasca River Basin based on Dynamically Downscaled Climate Scenarios of IPCC

Specialization: Water Resources Engineering Degree: Master of Science Abstract: To investigate the potential hydrologic impact of climate change on the Athabasca River Basin (ARB) of Alberta, Canada, the fully distributed physically based model, Modified Interactions Soil-Biosphere-Atmosphere (MISBA...

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Main Author: Wang, Jingwen
Other Authors: Gan, Thian Yew (Department of Civil and Environmental Engineering), Reuter, Gerhard (Department of Earth and Atmospheric Sciences), She, Yuntong (Department of Civil and Environmental Engineering)
Format: Thesis
Language:English
Published: University of Alberta. Department of Civil and Environmental Engineering. 2014
Subjects:
geo
Online Access:http://hdl.handle.net/10402/era.39479
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spelling fttriple:oai:gotriple.eu:10402/era.39479 2023-05-15T15:26:01+02:00 Potential Hydrologic Impact of Climate Change to Athabasca River Basin based on Dynamically Downscaled Climate Scenarios of IPCC Wang, Jingwen Gan, Thian Yew (Department of Civil and Environmental Engineering) Reuter, Gerhard (Department of Earth and Atmospheric Sciences) She, Yuntong (Department of Civil and Environmental Engineering) 2014-09-04 http://hdl.handle.net/10402/era.39479 en eng University of Alberta. Department of Civil and Environmental Engineering. 10402/era.39479 http://hdl.handle.net/10402/era.39479 undefined ERA : Education and Research Archive envir geo Thesis https://vocabularies.coar-repositories.org/resource_types/c_46ec/ 2014 fttriple 2023-01-22T17:07:03Z Specialization: Water Resources Engineering Degree: Master of Science Abstract: To investigate the potential hydrologic impact of climate change on the Athabasca River Basin (ARB) of Alberta, Canada, the fully distributed physically based model, Modified Interactions Soil-Biosphere-Atmosphere (MISBA) land surface scheme of Kerkhoven and Gan (2006) was driven with two SRES climate change scenarios (A1B and A2) of four General Circulation Models (GCMs) of IPCC (2007) dynamically downscaled by MM5, to simulate the future water availability of ARB for 2050s and 2080s. MM5 is the Fifth-generation Mesoscale Model jointly developed by the Pennsylvania State University (PSU) and the National Center for Atmospheric Research (NCAR). The four GCMs selected were ECHAM5 (wettest), MIROC3.2 (warmest and driest), CGCM3 and CCSM3 (moderate). Due to warming, the future streamflow of ARB simulated by MISBA show that ARB is generally expected to experience a decrease in streamflow. The management of ARB’s water resources system should be adjusted to augment against possible shortfall to various users relying on ARB for water supply. The results of this study based on climate scenarios of GCMs dynamically downscaled by MM5 are compared with results of Kerkhoven and Gan (2011) for ARB based on climate scenarios that were statistically downscaled. Thesis Athabasca River Unknown Athabasca River Canada
institution Open Polar
collection Unknown
op_collection_id fttriple
language English
topic envir
geo
spellingShingle envir
geo
Wang, Jingwen
Potential Hydrologic Impact of Climate Change to Athabasca River Basin based on Dynamically Downscaled Climate Scenarios of IPCC
topic_facet envir
geo
description Specialization: Water Resources Engineering Degree: Master of Science Abstract: To investigate the potential hydrologic impact of climate change on the Athabasca River Basin (ARB) of Alberta, Canada, the fully distributed physically based model, Modified Interactions Soil-Biosphere-Atmosphere (MISBA) land surface scheme of Kerkhoven and Gan (2006) was driven with two SRES climate change scenarios (A1B and A2) of four General Circulation Models (GCMs) of IPCC (2007) dynamically downscaled by MM5, to simulate the future water availability of ARB for 2050s and 2080s. MM5 is the Fifth-generation Mesoscale Model jointly developed by the Pennsylvania State University (PSU) and the National Center for Atmospheric Research (NCAR). The four GCMs selected were ECHAM5 (wettest), MIROC3.2 (warmest and driest), CGCM3 and CCSM3 (moderate). Due to warming, the future streamflow of ARB simulated by MISBA show that ARB is generally expected to experience a decrease in streamflow. The management of ARB’s water resources system should be adjusted to augment against possible shortfall to various users relying on ARB for water supply. The results of this study based on climate scenarios of GCMs dynamically downscaled by MM5 are compared with results of Kerkhoven and Gan (2011) for ARB based on climate scenarios that were statistically downscaled.
author2 Gan, Thian Yew (Department of Civil and Environmental Engineering)
Reuter, Gerhard (Department of Earth and Atmospheric Sciences)
She, Yuntong (Department of Civil and Environmental Engineering)
format Thesis
author Wang, Jingwen
author_facet Wang, Jingwen
author_sort Wang, Jingwen
title Potential Hydrologic Impact of Climate Change to Athabasca River Basin based on Dynamically Downscaled Climate Scenarios of IPCC
title_short Potential Hydrologic Impact of Climate Change to Athabasca River Basin based on Dynamically Downscaled Climate Scenarios of IPCC
title_full Potential Hydrologic Impact of Climate Change to Athabasca River Basin based on Dynamically Downscaled Climate Scenarios of IPCC
title_fullStr Potential Hydrologic Impact of Climate Change to Athabasca River Basin based on Dynamically Downscaled Climate Scenarios of IPCC
title_full_unstemmed Potential Hydrologic Impact of Climate Change to Athabasca River Basin based on Dynamically Downscaled Climate Scenarios of IPCC
title_sort potential hydrologic impact of climate change to athabasca river basin based on dynamically downscaled climate scenarios of ipcc
publisher University of Alberta. Department of Civil and Environmental Engineering.
publishDate 2014
url http://hdl.handle.net/10402/era.39479
geographic Athabasca River
Canada
geographic_facet Athabasca River
Canada
genre Athabasca River
genre_facet Athabasca River
op_source ERA : Education and Research Archive
op_relation 10402/era.39479
http://hdl.handle.net/10402/era.39479
op_rights undefined
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