Spatial and temporal dynamics of groundwater flow across a wet meadow, Polar Bear Pass, Bathurst island, Nunavut

• Published in: Permafrost and Periglacial Processes
• Main Authors: Kathy L. Young, Harold‐Alexis Scheffel, Anna Abnizova, John R. Siferd
• Format: Article in Journal/Newspaper
• Language: unknown
• Subjects: Bathurst Island; Bear Pass; Nunavut; Polar Bear Pass; Tundra
• Online Access: https://doi.org/10.1002/ppp.1931

Interest is growing about how groundwater supplies will shift in warming northern terrains. We evaluated the seasonal and spatial pattern of groundwater flow in a wet meadow bordered by a late‐lying snowbed and tundra ponds at Polar Bear Pass, Bathurst Island (75.7°N, 98.7°W). A water budget approach signalled the relative importance of groundwater inflow to tundra ponds. Groundwater flow across the wet meadow was estimated using a modified Darcy's equation, which requires information on both water and frost tables, and hydraulic conductivity. These data were obtained from 2007 to 2009 along a series of water wells extending from a late‐lying snowbed across the wet meadow to a nearby study pond. Groundwater fluxes across the wet meadow were limited in magnitude and duration in a warm/dry year (2007), when the late‐lying snowbed was the main external water source, a response differing from rainy/cool years (2008 and 2009). Overall, seasonal water budgets indicate that groundwater fluxes were minimal in the wet meadow and an adjacent tundra pond. Late‐lying snowbeds play a limited role in sustaining wet meadows and ponds here. Summer precipitation and evaporation continue to drive wet meadow and tundra pond hydrological response in low‐gradient wetlands, especially in the post‐snowmelt season. Copyright © 2016 John Wiley & Sons, Ltd.