Sea ice local surface topography from single-pass satellite InSAR measurements: a feasibility study
Other literature type, Article
- Publisher: Copernicus Publications
(issn: 1994-0424, eissn: 1994-0424)
VDP::Mathematics and natural science: 400::Physics: 430 | GE1-350 | QE1-996.5 | Environmental sciences | VDP::Matematikk og Naturvitenskap: 400::Fysikk: 430 | Geology
Palsas and peat plateaus are permafrost landforms occurring in subarctic
mires which constitute sensitive ecosystems with strong significance for
vegetation, wildlife, hydrology and carbon cycle. Firstly, we have systematically mapped the occurrence of palsas and peat plateaus in the northernmost county of Norway (Finnmark, ∼ 50 000 km<sup>2</sup>) by manual interpretation of aerial images from 2005 to 2014 at a spatial resolution of 250 m. At this resolution, mires and wetlands with palsas or peat plateaus occur in about 850 km<sup>2</sup> of Finnmark, with the actual palsas and peat plateaus underlain by permafrost covering a surface area of approximately 110 km<sup>2</sup>. Secondly, we have quantified the lateral changes of the extent of palsas and peat plateaus for four study areas located along a NW–SE transect through Finnmark by utilizing repeat aerial imagery from the 1950s to the 2010s. The results of the lateral changes reveal a total decrease of 33–71 % in the areal extent of palsas and peat plateaus during the study period, with the largest lateral change rates observed in the last decade. However, the results indicate that degradation of palsas and peat plateaus in northern Norway has been a consistent process during the second half of the 20th century and possibly even earlier. Significant rates of areal change are observed in all investigated time periods since the 1950s, and thermokarst landforms observed on aerial images from the 1950s suggest that lateral degradation was already an ongoing process at this time. The results of this study show that lateral erosion of palsas and peat plateaus is an important pathway for permafrost degradation in the sporadic permafrost zone in northern Scandinavia. While the environmental factors governing the rate of erosion are not yet fully understood, we note a moderate increase in air temperature, precipitation and snow depth during the last few decades in the region.