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Simulating the impact of climate change on the groundwater resources of the Magdalen Islands, Québec, Canada
Author(s) -
JeanMichel Lemieux,
Jalil Hassaoui,
John Molson,
René Therrien,
Pierre Therrien,
Michel Chouteau,
Michel Ouellet
Publication year - 2015
Publication title -
journal of hydrology regional studies
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.573
H-Index - 36
ISSN - 2214-5818
DOI - 10.1016/j.ejrh.2015.02.011
Subject(s) - groundwater recharge , archipelago , groundwater , hydrology (agriculture) , climate change , environmental science , oceanography , geography , water resources , erosion , natural (archaeology) , geology , aquifer , ecology , geomorphology , archaeology , geotechnical engineering , biology
tudy regionThis study is conducted in the Magdalen Islands (Québec, Canada), a small archipelago located in the Gulf of St. Lawrence.Study focusThis work was undertaken to support the design of a long-term groundwater monitoring network and for the sustainable management of groundwater resources. This study relies mostly on the compilation of existing data, but additional field work has also been carried out, allowing for the first time in the Magdalen Islands, direct observation of the depth and shape of the transition zone between freshwater and seawater under natural conditions. Simulations were conducted along a 2D cross-section on Grande Entrée Island in order to assess the individual and combined impacts of sea-level rise, coastal erosion and decreased groundwater recharge on the position of the saltwater–freshwater interface. The simulations were performed considering variable-density flow and solute transport under saturated-unsaturated conditions. The model was driven by observed and projected climate change scenarios to 2040 for the Magdalen Islands.New hydrological insights for the regionThe simulation results show that among the three impacts considered, the most important is sea-level rise, followed by decreasing groundwater recharge and coastal erosion. When combined, these impacts cause the saltwater–freshwater interface to migrate inland over a distance of 37m and to rise by 6.5m near the coast to 3.1m further inland, over a 28-year period

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