Impacts of climate change on streamflow in the McKenzie Creek watershed in the Great Lakes region

Frontiers in Environmental Science

Environmental Science

Dawn Martin-Hill¹  Olivier Champagne²  Patricia Chow-Fraser³  M. Altaf Arain⁴  Tariq A. Deen⁴ 

[1] Department of Anthropology, McMaster University, Hamilton, ON, Canada;Institut des Géosciences de l’Environnement, Université Grenoble Alpes, Centre National de la Recherche Scientifique (CNRS), Grenoble, France;McMaster Centre for Climate Change, McMaster University, Hamilton, ON, Canada;Department of Biology, McMaster University, Hamilton, ON, Canada;School of Earth, Environment and Society, McMaster University, Hamilton, ON, Canada;McMaster Centre for Climate Change, McMaster University, Hamilton, ON, Canada;

关键词: climate change;    climate change impacts;    hydrology;    streamflow;    GSFLOW integrated hydrologic model;    Six Nations of the Grand River;    Indigenous;   

DOI  :  10.3389/fenvs.2023.1171210

 received in 2023-02-21, accepted in 2023-05-15,  发布年份 2023

来源: Frontiers

【 摘 要 】

Introduction: This study explored streamflow dynamics of the McKenzie Creek watershed in Southern Ontario, Canada under a changing climate. The Creek is located in the southern portion of the Grand River watershed in the Great Lakes region and is an important water and ecosystem service provider for the Six Nations of the Grand River reserve, the largest (by population) Indigenous community in Canada and the fourth largest in North America.Methods: The Coupled Groundwater and Surface-Water Flow Model (GSFLOW) was used to simulate streamflow from 1951 to 2020 using observed gridded meteorological data from Natural Resources Canada (NRCANmet) and in situ data from Environment and Climate Change Canada (ECCC). Downscaled data from the Coupled Model Intercomparison Project Phase 5 (CMIP5) for two Intergovernmental Panel on Climate Change (IPCC) Representative Concentration Pathways (RCP) climate warming scenarios, RCP 4.5 and RCP 8.5 were used to run GSFLOW for the historic (1951–2020) and projected (2021–2099) period.Results: Results suggested that streamflow in the McKenzie Creek will be significantly impacted by climate change in winter months when streamflow is projected to increase due to higher temperatures causing early melting of snowpack and increasing winter precipitation. Consequently, spring streamflow is expected to decrease and little or no change in streamflow in the summer and autumn. These changes in streamflow dynamics may lead to more flooding incidents in the winter, while at the same time, the region may face reduced water availability or dry conditions in late spring and summer due to warm temperatures.Discussion: This study provides important information about streamflow and hydrologic dynamics of this watershed that will help managers and planners to better manage water resources and be prepared to deal with climate change and its impacts on water availability and security not only for the Six Nations area but also for Southern Ontario which houses one-third of Canada’s population.

【 授权许可】

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Copyright © 2023 Deen, Arain, Champagne, Chow-Fraser and Martin-Hill.