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The role of snow processes and hillslopes on runoff generation in present and future climates in a recently constructed watershed in the Athabasca oil sands region
  • Kelly Biagi,
  • Sean Carey
Kelly Biagi
McMaster University

Corresponding Author:[email protected]

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Sean Carey
McMaster University
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Mine reclamation in the Athabasca oil sands region Canada, is required by law where companies must reconstruct disturbed landscapes into functioning ecosystems such as forests, wetlands and lakes that existed in the Boreal landscape prior to mining. Winter is a major hydrological factor in this region as snow covers the landscape for 5 to 6 months and is ~25% of the annual precipitation, yet few studies have explored the influence of winter processes on the hydrology of constructed watersheds. One year (2017-2018) of intensive snow hydrology measurements are supplemented with six years (2013-2018) of meteorological measurements from the constructed Sandhill Fen Watershed to: 1) understand snow accumulation and redistribution, snowmelt timing, rate and partitioning, 2) apply a physically-based model for simulating winter processes on hillslopes and 3) evaluate the impact of soil prescriptions and climate change projections on winter processes in reclaimed systems. The 2017-2018 snow season was between November and April and SWE ranged between 40-140 mm. Snow distribution was primarily influenced by topography with little influence of snow trapping from developing vegetation. Snow accumulation was most variable on hillslopes and redistribution was driven by slope position, with SWE greatest at the base of slopes and decreased towards crests. Snowmelt on hillslopes was controlled by slope aspect, as snow declined rapidly on west and south-facing slopes, compared to east and north-facing slopes. Unlike results previously reported on constructed uplands, snowmelt runoff from uplands was much less (~30%), highlighting the influence of different construction materials. Model simulations indicate that antecedent soil moisture and soil temperature have a large influence on partitioning snowmelt over a range of observed conditions. Under a warmer and wetter climate, average annual peak SWE and snow season duration could decline up to 52 % and up to 61 days, respectively while snowmelt runoff ceases completely under the warmest scenarios. Results suggest considerable future variability in snowmelt runoff from hillslopes, yet soil properties can be used to enhance vertical or lateral flows.
18 Mar 2020Submitted to Hydrological Processes
21 Mar 2020Submission Checks Completed
21 Mar 2020Assigned to Editor
21 Mar 2020Reviewer(s) Assigned
24 Apr 2020Review(s) Completed, Editorial Evaluation Pending
25 Apr 2020Editorial Decision: Revise Major
22 May 20201st Revision Received
25 May 2020Reviewer(s) Assigned
25 May 2020Submission Checks Completed
25 May 2020Assigned to Editor
25 May 2020Review(s) Completed, Editorial Evaluation Pending
25 May 2020Editorial Decision: Accept
15 Aug 2020Published in Hydrological Processes volume 34 issue 17 on pages 3635-3655. 10.1002/hyp.13836