A synthesis of thermokarst lake water balance in high-latitude regions of North America from isotope tracers

dc.contributor.authorMacDonald, Lauren A.
dc.contributor.authorWolfe, Brent B.
dc.contributor.authorTurner, Kevin W.
dc.contributor.authorAnderson, Lesleigh
dc.contributor.authorArp, Christopher D.
dc.contributor.authorBirks, S. Jean
dc.contributor.authorBouchard, Frédéric
dc.contributor.authorEdwards, Thomas W.D.
dc.contributor.authorFarquharson, Nicole
dc.contributor.authorHall, Roland I.
dc.contributor.authorMcDonald, Ian
dc.contributor.authorNarancic, Biljana
dc.contributor.authorOuimet, Chantal
dc.contributor.authorPienitz, Reinhard
dc.contributor.authorTondu, Jana
dc.contributor.authorWhite, Hilary
dc.date.accessioned2018-08-27T13:57:59Z
dc.date.available2018-08-27T13:57:59Z
dc.date.copyright2017en_US
dc.date.issued2017
dc.description.abstractNumerous studies utilizing remote sensing imagery and other methods have documented that thermokarst lakes are undergoing varied hydrological transitions in response to recent climate changes, from surface area expansion to drainage and evaporative desiccation. Here, we provide a synthesis of hydrological conditions for 376 lakes of mainly thermokarst origin across high-latitude North America. We assemble surface water isotope compositions measured during the past decade at five lake-rich landscapes including Arctic Coastal Plain (Alaska), Yukon Flats (Alaska), Old Crow Flats (Yukon), northwestern Hudson Bay Lowlands (Manitoba), and Nunavik (Quebec). These landscapes represent the broad range of thermokarst environments by spanning gradients in meteorological, permafrost, and vegetation conditions. An isotope framework was established based on flux-weighted long-term averages of meteorological conditions for each lake to quantify water balance metrics. The isotope composition of source water and evaporation-to-inflow ratio for each lake were determined, and the results demonstrated a substantial array of regional and subregional diversity of lake hydrological conditions. Controls on lake water balance and how these vary among the five landscapes and with differing environmental drivers are assessed. Findings reveal that lakes in the Hudson Bay Lowlands are most vulnerable to evaporative desiccation, whereas those in Nunavik are most resilient. However, we also identify the complexity in predicting hydrological responses of these thermokarst landscapes to future climate change.en_US
dc.description.reviewstatusRevieweden_US
dc.description.scholarlevelFacultyen_US
dc.description.sponsorshipWe would like to thank the many funding agencies and organizations that support our research as well as the many assistants in the field. This is a contribution to the NSERC Discovery Frontiers program, Arctic Development and Adaptation to Permafrost in Transition (ADAPT). Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the US Government.en_US
dc.identifier.citationMacDonald, L.A.; Wolfe, B.B.; Turner, K.W.; Anderson, L.; Arp, C.D.; Birks, S.J.; … & White, H. (2017). A synthesis of thermokarst lake water balance in high-latitude regions of North America from isotope tracers. Arctic Science, 3(2), 118-149. https://doi.org/10.1139/as-2016-0019en_US
dc.identifier.urihttps://doi.org/10.1139/as-2016-0019
dc.identifier.urihttp://hdl.handle.net/1828/9954
dc.language.isoenen_US
dc.publisherArctic Scienceen_US
dc.subjectthermokarst lakes
dc.subjecthigh-latitude regions
dc.subjectwater isotope tracers
dc.subjecthydrology
dc.subjectpermafrost
dc.subjectclimate change
dc.subject.departmentDepartment of Geography
dc.titleA synthesis of thermokarst lake water balance in high-latitude regions of North America from isotope tracersen_US
dc.typeArticleen_US

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