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Changing groundwater discharge dynamics in permafrost regions

Bibliographic Data

ID15545293
AuthorsPierrick Lamontagne‐Hallé (0000-0001-7831-7145, McGill University, corresponding author), Jeffrey M McKenzie (0000-0002-0469-6469, McGill University), Barret L Kurylyk (0000-0002-8244-3838, Dalhousie University), Samuel C Zipper (0000-0002-8735-5757, University of Victoria)
Year2018
Volume13
Issue8
Pages084017-084017
Publication date2018-07-17
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueEnvironmental Research Letters (JOURNAL)
Journal identifiersISSN: 1748-9326 • E-ISSN: 1748-9326
PublisherIOP Publishing (PUBLISHER • GB)
DOI10.1088/1748-9326/aad404
OpenAlexW2883481102
LanguageEN
Citations received7
References cited47

Permafrost thaw due to climate warming modifies hydrological processes by increasing hydrological connectivity between aquifers and surface water bodies and increasing groundwater storage. While previous studies have documented arctic river baseflow increases and changing wetland and lake distributions, the hydrogeological processes leading to these changes remain poorly understood. This study uses a coupled heat and groundwater flow numerical model with dynamic freezing and thawing processes and an improved set of boundary conditions to simulate the impacts of climate warming on permafrost distribution and groundwater discharge to surface water bodies. We show a spatial shift in groundwater discharge from upslope to downslope and a temporal shift with increasing groundwater discharge during the winter season due to the formation of a lateral supra-permafrost talik underlying the active layer. These insights into changing patterns of groundwater discharge help explain observed changes in arctic baseflow and wetland patterns and are important for northern water resources and ecosystem management

Aquifer · Arctic · Baseflow · Climate change · Discharge · Drainage basin · Geography · Groundwater · Groundwater discharge · Groundwater flow · Hydrogeology · Hydrology (agriculture · Permafrost · Streamflow · Surface water · Thermokarst · Water table · Wetland · Arctic and Antarctic ice dynamics · Climate change and permafrost · Cryospheric studies and observations · Environmental Science · Ecology · Geology · Oceanography

  • Water balance response of permafrost-affected watersheds to changes in air temperatures

    Open Access•Matvey Debolskiy, V A Alexeev et al.•Environmental Research Letters•2021

  • Increasing annual streamflow and groundwater storage in response to climate warming in the Yangtze River source region

    Open Access•Wenxuan Yi, Yuqing Feng et al.•Environmental Research Letters•2021

  • Recent regional warming across the Siberian lowlands

    Open Access•Ping Wang, Qiwei Huang et al.•Environmental Research Letters•2022

  • Classifying pan-Arctic supra-permafrost aquifer function under present and projected conditions

    Open Access•Bay Berry, Julia Guimond et al.•Environmental Research Letters•2026

  • Potential role of permafrost thaw on increasing Siberian river discharge

    Open Access•Ping Wang, Qiwei Huang et al.•Environmental Research Letters•2021

  • Sea-level rise and warming mediate coastal groundwater discharge in the Arctic

    Open Access•Julia Guimond, Aaron A Mohammed et al.•Environmental Research Letters•2022

  • Wind-modulated groundwater discharge along a microtidal Arctic coastline

    Open Access•Julia Guimond, Cansu Demir et al.•Environmental Research Letters•2023

  • Disappearing Arctic Lakes

    Open Access•Laura C Smith, Yongwei Sheng et al.•Science•2005

  • Estimation of the residence time of permafrost groundwater in the middle of the Lena River basin, eastern Siberia

    Open Access•Tetsuya Hiyama, Kazuyoshi Asai et al.•Environmental Research Letters•2013

Unique citing works7
Citations per year1,4
Citation span2021 - 2026 (6)
Citation velocitycurrent
Highly citedNo
Citation typesNeutral: 7

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