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Monitoring of permafrost has been ongoing since 1978 in the Abisko area, northernmost Sweden, when measurements of active layer thickness started. In 1980, boreholes were drilled in three mires in the area to record permafrost temperatures. Recordings were made twice per year, and the last data were obtained in 2002. During the International Polar Year (2007-2008), new boreholes were drilled within the 'Back to the Future' (BTF) and 'Thermal State of Permafrost' (TSP) projects that enabled year-round temperature monitoring. Mean annual ground temperatures (MAGT) in the mires are close to 0°C, ranging from −0.16 to −0.47°C at 5 m depth. Data from the boreholes show increasing ground temperatures in the upper and lower part by 0.4 to 1°C between 1980 and 2002. At one mire, permafrost thickness has decreased from 15 m in 1980 to ca. 9 m in 2009, with an accelerating thawing trend during the last decade. [ABSTRACT FROM AUTHOR]

The article discusses the results of research regarding mountain permafrost developments in the Abisko area of northern Sweden. Results indicate the occurrence of permafrost as varying greatly over short distances in the Abisko area. The author concludes that arctic permafrost and mountain permafrost can be identified in the Abisko area. Both types are associated with the current climate in the area, have an active character, and are of sporadic form.