Mechanisms of Discontinuous Permafrost Thaw in Peatlands

Climate warming in discontinuous permafrost peatlands is causing permafrost loss and changes in ecosystem dynamics at an unprecedented rate. Though rates of permafrost loss and landscape change have been widely documented based on remote sensing and field measurements, the local mechanisms of permafrost degradation remain under-studied. These mechanisms were explored using data collected over three decades of research in the Scotty Creek study basin in the southern Northwest Territories of Canada. The data, when compared to numerical modeling results, demonstrated that vertical heat conduction accounts for most vertical permafrost degradation, while advective heat transfer drives thaw in features which are subject to seasonal flows. It was found that heat advection was necessary to describe lateral thaw rates of up to 115 cm annually, which are an order of magnitude greater than vertical thaw rates, which average 10 cm annually. Thaw from below, driven either by the geothermal gradient or groundwater flow, may account for up to 10 cm of permafrost thaw annually. The hydrologic, thermodynamic and geophysical function of taliks in different parts of the landscape were considered in light of the data collected at the field site and surrounding area. This analysis is supported through the use of ERT data detailing the subsurface permafrost structure. This understanding of local thaw mechanisms and trajectory is an important first step in being able to predict distributed permafrost thaw in peatlands.

Automated summary

The study found that in discontinuous permafrost peatlands, thaw rates are faster compared to other regions, and vertical heat conduction and advective heat transfer play crucial roles in the thawing process. Additionally, geothermal gradient and groundwater flow may also contribute to permafrost thaw. Analyzing the functions of taliks in different landscapes can provide insights into the subsurface permafrost structure.