Isotopic tracing of hydrologic drivers including permafrost thaw status for lakes across Northeastern Alberta, Canada: A 16-year, 50-lake assessment

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dc.contributor.authorGibson, J.J.
dc.contributor.authorYib, Y.
dc.contributor.authorBirks, S.J.
dc.date.accessioned2020-02-14T00:59:08Z
dc.date.available2020-02-14T00:59:08Z
dc.date.copyright2019en_US
dc.date.issued2019
dc.description.abstractStudy region Surveys of stable isotopes of water in 50 boreal lakes were conducted during 2002–2017 as a component of Alberta’s Oil Sands acid sensitivity program in northeastern Alberta. Study focus Using an isotope mass balance approach, watershed, climatic and isotopic data were applied to estimate evaporation losses and residence time of lakes, as well as to estimate water yield from watersheds. New hydrological insights for the region Site-specific differences in water yield to 50 lakes over 16 years were found to be controlled by latitudinal gradients in climate, wetland type, lake/watershed configuration and permafrost. 19 plateau watersheds located northeast of Fort McMurray and in the Birch and Caribou Mountains which contained significant permafrost were found to have similar water yield to permafrost-poor watersheds if fen-dominated (159 mm/yr: n = 5 vs. 166 mm/yr; n = 31), and enhanced water yield (405 mm/yr; n = 14) if bog-dominated. Water yield was found to be systematically dependent on permafrost extent, yielding up to several hundred millimetres of additional runoff in bog-dominated systems. Temporal trend analysis indicates systemic momentum of change in hydrologic drivers over the 16-year period, although few are statistically significant. A new conceptual framework is proposed for classification of site-to-site permafrost thaw stage to improve water yield prediction, which is expected to influence lake water quality including observed pH increases noted previously for many lakes in the region.en_US
dc.description.reviewstatusRevieweden_US
dc.description.scholarlevelFacultyen_US
dc.description.sponsorshipFunding for the hydrological assessment was obtained through grants to JJG from InnoTech Alberta, the Cumulative Environmental Management Association (CEMA), Alberta Environment and Parks, and Natural Sciences and Engineering Research Council of Canada (Discovery and Collaborative Research and Development CRDPJ 357130 – 07).en_US
dc.identifier.citationGibson, J.J., Yib, Y. & Birks, S.J. (2019). Isotopic tracing of hydrologic drivers including permafrost thaw status for lakes across Northeastern Alberta, Canada: A 16-year, 50-lake assessment. Journal of Hydrology: Regional Studies, 26, 100643. https://doi.org/10.1016/j.ejrh.2019.100643en_US
dc.identifier.urihttps://doi.org/10.1016/j.ejrh.2019.100643
dc.identifier.urihttp://hdl.handle.net/1828/11553
dc.language.isoenen_US
dc.publisherJournal of Hydrology: Regional Studiesen_US
dc.subjectIsotopes
dc.subjectLakes
dc.subjectWater balance
dc.subjectEvaporation
dc.subjectBoreal
dc.subjectBog
dc.subjectFen
dc.subjectPermafrost thaw
dc.subject.departmentDepartment of Geography
dc.titleIsotopic tracing of hydrologic drivers including permafrost thaw status for lakes across Northeastern Alberta, Canada: A 16-year, 50-lake assessmenten_US
dc.typeArticleen_US

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