Influence of vertical and lateral heat transfer on permafrost thaw, peatland landscape transition, and groundwater flow

• Published in: Water resources research 2016-02, Vol.52 (2), p.1286-1305
• Main Authors: Kurylyk, Barret L., Hayashi, Masaki, Quinton, William L., McKenzie, Jeffrey M., Voss, Clifford I.
• Format: Article
• Language: English
• Subjects: Boreal forests; Boundary conditions; Climate change; Climatic data; Energy balance; Flow rates; Flow system; Groundwater; Groundwater flow; heat advection; Heat transfer; Landscape; landscape evolution; Peat; peatland; Permafrost; Plateaus; soil freeze‐thaw; Soil surfaces; Soil temperature; Stream discharge; Stream flow; Subsurface water; Surface flow; Surface temperature; Water flow; Wetlands
• ISSN: 0043-1397; 1944-7973
• DOI: 10.1002/2015WR018057

Recent climate change has reduced the spatial extent and thickness of permafrost in many discontinuous permafrost regions. Rapid permafrost thaw is producing distinct landscape changes in the Taiga Plains of the Northwest Territories, Canada. As permafrost bodies underlying forested peat plateaus shrink, the landscape slowly transitions into unforested wetlands. The expansion of wetlands has enhanced the hydrologic connectivity of many watersheds via new surface and near‐surface flow paths, and increased streamflow has been observed. Furthermore, the decrease in forested peat plateaus results in a net loss of boreal forest and associated ecosystems. This study investigates fundamental processes that contribute to permafrost thaw by comparing observed and simulated thaw development and landscape transition of a peat plateau‐wetland complex in the Northwest Territories, Canada from 1970 to 2012. Measured climate data are first used to drive surface energy balance simulations for the wetland and peat plateau. Near‐surface soil temperatures simulated in the surface energy balance model are then applied as the upper boundary condition to a three‐dimensional model of subsurface water flow and coupled energy transport with freeze‐thaw. Simulation results demonstrate that lateral heat transfer, which is not considered in many permafrost models, can influence permafrost thaw rates. Furthermore, the simulations indicate that landscape evolution arising from permafrost thaw acts as a positive feedback mechanism that increases the energy absorbed at the land surface and produces additional permafrost thaw. The modeling results also demonstrate that flow rates in local groundwater flow systems may be enhanced by the degradation of isolated permafrost bodies. Key Points: Observed permafrost thaw rates are compared to results from a 3‐D groundwater flow and heat transfer model Lateral heat flow can accelerate discontinuous permafrost thaw and land cover change in peatlands Degradation of discontinuous permafrost enhances local groundwater flow