<p>This thesis outlines the development and decay of palsas in northern Sweden in relation to climatic and environmental factors. Palsas were investigated on morphology, vegetation, peat porosity, ground temperature and local climate in four bogs situated on a north-south gradient in northern Sweden. A new classification for palsa stages (embryo, young, mature, degrading and remnant stage), based on morphological and vegetational characteristics, is proposed and described in the thesis. The start of palsa growth seems to be favoured by a low vegetation height and a high cover of <i>Sphagnum</i> mosses. Very high porosities were measured in this peat type, resulting in a high insulation capacity preserving the frozen ground in summer. A decrease of porosities in the surface peat layer from the embryo palsa stage to the mature and degrading palsa stage was found. This contributes to the degrading of palsas, due to higher thermal diffusivities in palsas with lower porosities. The aggradation of the ice core can also cease due to the observed change in vegetation from low vegetation on embryo and young palsas to vegetation with tall <i>Betula nana</i> shrubs on degrading palsas. This was found to cause thicker snow cover that prevents frost penetration into the palsa core. The present climate conditions (with mean annual temperature of –1.5°C and annual precipitation of 737 mm) at the boundary of palsa distribution in Sweden were found to be unsuitable for palsa development. Palsa growth started here during a cold period in the last part of the Little Ice Age, with estimated mean annual and mean winter temperatures of –2.3°C and –10.0°C, respectively. </p><p>The major conclusions are that besides air temperature, depth of snow cover, summer precipitation and hydrology, also vegetation cover and peat characteristics are important for palsa growth and decay.</p>

This thesis outlines the development and decay of palsas in northern Sweden in relation to climatic and environmental factors. Palsas were investigated on morphology, vegetation, peat porosity, ground temperature and local climate in four bogs situated on a north-south gradient in northern Sweden. A new classification for palsa stages (embryo, young, mature, degrading and remnant stage), based on morphological and vegetational characteristics, is proposed and described in the thesis. The start of palsa growth seems to be favoured by a low vegetation height and a high cover of Sphagnum mosses. Very high porosities were measured in this peat type, resulting in a high insulation capacity preserving the frozen ground in summer. A decrease of porosities in the surface peat layer from the embryo palsa stage to the mature and degrading palsa stage was found. This contributes to the degrading of palsas, due to higher thermal diffusivities in palsas with lower porosities. The aggradation of the ice core can also cease due to the observed change in vegetation from low vegetation on embryo and young palsas to vegetation with tall Betula nana shrubs on degrading palsas. This was found to cause thicker snow cover that prevents frost penetration into the palsa core. The present climate conditions (with mean annual temperature of –1.5°C and annual precipitation of 737 mm) at the boundary of palsa distribution in Sweden were found to be unsuitable for palsa development. Palsa growth started here during a cold period in the last part of the Little Ice Age, with estimated mean annual and mean winter temperatures of –2.3°C and –10.0°C, respectively. The major conclusions are that besides air temperature, depth of snow cover, summer precipitation and hydrology, also vegetation cover and peat characteristics are important for palsa growth and decay.

Electrical resistivity tomography (ERT) is a commonly used geophysical method to investigate permafrost in the mountain environment, but few studies have employed this method in a permafrost affected peatland. For this thesis, 5 ERT profiles were measured over 17 palsas and peat-plateaus in a palsa peatland environment in Tavvavuoma, northern Sweden, where the primary aim was to investigate the depth to the base of permafrost under the mounds. These depths are also used to estimate the excess ice fraction (EIF), which is indicative of the proportion of segregation ice in the frozen core under the mounds. The internal structure of palsas and the spatial distribution of permafrost was also investigated from the inverted resistivity models. Permafrost thickness was found to range from 5 – 17 m, with the thickest permafrost in the west end of the study area. EIF values range between 0,04 to 0,58, with the lowest values in the same end as the deepest permafrost, where also low mound elevations are found. The deep permafrost combined with low mound elevations are suggested to be attributed to the presence of coarse grained (glaciofluvial) sediments where ice segregation formation is limited, thus small amounts of frost heave. Deep permafrost is possibly underlying at least two thermokarst depressions/fens in the area, which is suggested to obstruct their drainage. The height of the mounds was surprisingly found to decrease with permafrost thickness, a relationship that is likely to be an effect of the varied underlying sediment cover. This thesis demonstrates the applicability of ERT in peatland permafrost research, but also considers the limitations of the method. / Elektrisk resistivitetstomografi (ERT) är en geofysisk metod som har använts flitigt vid undersökningar av alpin permafrost, men få studier har hittills tillämpat denna teknik vid undersökningar av permafrost i myrmarker. Under detta examensarbete på masternivå mättes 5 ERT-profiler över 17 palsar samt torvplatåer i ett palsmyrkomplex med sporadisk permafrost i Tavvavuoma, norra Sverige, med det primära målet att undersöka permafrostens mäktighet under dessa. De beräknade permafrostdjupen används även för att uppskatta isöverskottsfraktionen (EIF), vilket ger en indikation på andelen segregationsis i den frusna kärnan under respektive pals/torvplatå. Palsarnas interna struktur och den rumsliga utbredningen av permafrost i myren diskuteras också kvalitativt utifrån resistivitetsmodellerna. Permafrostmäktigheten under palsar och torvplatåer bestämdes till mellan 5 – 17 meter, med den djupaste permafrosten i den västra delen av studieområdet. Isöverskottsfraktionen varierar mellan 0,04 – 0,58, med de lägsta värdena i samma del av studieområdet som den djupaste permafrosten fanns, här är även palshöjderna låga. Den djupa permafrosten i kombination med låga palshöjder föreslås tillskrivas förekomst av grovkorniga (glaciofluviala) sediment i denna del av studieområdet, där bildningen av segregationsis begränsas. I och med detta begränsas mängden frosthävning, med låga palshöjder som resultat. Djup permafrost kan finnas under minst två thermokarstsänkor i området, vilket kan hindra dränering av dessa. Ett oväntat resultat var att palshöjd minskar med ökat permafrostdjup bland de studerade objekten, vilket bäst kan förklaras med det varierade sedimentunderlaget, som ger mycket olika förutsättningar för segregationsisbildning. Denna masteruppsats visar på tillämpligheten av ERT i myrmarker med permafrost, men beaktar även metodens begränsningar för denna tillämpning.