Preprints
https://doi.org/10.5194/egusphere-2022-1173
https://doi.org/10.5194/egusphere-2022-1173
 
14 Dec 2022
14 Dec 2022
Status: this preprint is open for discussion.

Permafrost degradation at two monitored palsa mires in north-west Finland

Mariana Verdonen1, Alexander Störmer2,4, Pasi Korpelainen1,4, Eliisa Lotsari1,3, Benjamin Burkhard2,4, Alfred Colpaert1, and Timo Kumpula1,4 Mariana Verdonen et al.
  • 1Department of Geographical and Historical Studies, University of Eastern Finland, Joensuu, 80101, Finland
  • 2Institute of Physical Geography and Landscape Ecology, Leibniz University Hannover, Hannover, 30167, Germany
  • 3Water and Environmental Engineering, Department of Built Environment, Aalto University, Aalto, 00076, Finland
  • 4Kilpisjärvi Biological Station, University of Helsinki, Kilpisjärvi, 99490, Finland

Abstract. Palsas and peat plateaus are expected to disappear from many regions, including Finnish Lapland. However, detailed long-term monitoring data of the degradation process on palsas are scarce. Here, we present the results of the aerial photography time series analysis (1960–2021) and annual RTK-GNSS and active layer monitoring (2007–2021) at two palsa sites (Peera and Laassaniemi) located in north-west Finland. The emphasis is on detailed change detection for the period covered by Unmanned Aerial System surveys (2016–2021) and connections to climate . At both sites, the decrease in palsa area by -77 % to -90 % since 1960 and height by -16 % to -49 % since 2007 indicate substantial permafrost degradation throughout the study periods . The area loss rates are mainly connected to winter air temperature changes at Peera and winter precipitation changes at Laassaniemi. The active layer thickness (ALT) has varied each year with no significant trend and is related mainly to snow depths and summer air temperatures at Peera. At Laassaniemi, the ALT is weakly related to climate and has been decreasing in the middle part of the palsa during the past eight years despite the continuous decrease in palsa volume. Our findings imply that the ALT in the inner parts of palsas do not necessarily reflect the overall permafrost conditions and underline the importance of surface position monitoring alongside the active layer measurements. The results also showed a negative relationship between the ALT and snow cover onset, indicating the complexity of climate–permafrost feedbacks in palsa mires.

Mariana Verdonen et al.

Status: open (until 18 Feb 2023)

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  • RC1: 'Comment on egusphere-2022-1173', Heather Reese, 15 Jan 2023 reply

Mariana Verdonen et al.

Mariana Verdonen et al.

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Short summary
The study revealed stable and even decreasing thickness of thaw depth in peat mounds with perennially frozen core, despite overall rapid permafrost degradation within 14 years. This means that measuring the thickness of thawed layer – a commonly used method – is alone insufficient to assess the permafrost conditions in subarctic peatlands. The study showed also that climate change is the main driver of these permafrost features’ decay, but its effect depends on peatland’s local conditions.