A synthesis of thermokarst lake water balance in high-latitude regions of North America from isotope tracers
Numerous 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 hydrol...
| Published in: | Arctic Science |
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| Main Authors: | , , , , , , , , , , , , , , , |
| Format: | Article in Journal/Newspaper |
| Language: | English |
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Arctic Science
2017
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| Subjects: | |
| Online Access: | https://doi.org/10.1139/as-2016-0019 https://dspace.library.uvic.ca//handle/1828/9954 |
| Summary: | Numerous 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. We 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. Faculty Reviewed |
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