In: Systematic Biology, 2017, vol. 66, no. 1, p. 3-22
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In: International Journal of Earth Sciences, 2015, vol. 104, no. 5, p. 1337-1352
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In: Pure and Applied Geophysics, 2015, vol. 172, no. 2, p. 545-568
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In: Journal of Soils and Sediments, 2015, vol. 15, no. 6, p. 1400-1419
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In: Journal Of Heredity, 2016, vol. 107, no. 5, p. 392-402
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In: Vegetation History and Archaeobotany, 2015, vol. 24, no. 2, p. 303-317
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In: Population and Environment, 2015, vol. 36, no. 4, p. 480-496
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In: Permafrost and Periglacial Processes, 2020, vol. 32, no. 1, p. 139-153
The ongoing acceleration in rock glacier velocities concurrent with increasing air temperatures, and the widespread onset of rock glacier destabilization have reinforced the interest in rock glacier dynamics and in its coupling to the climate system. Despite the increasing number of studies investigating this phenomenon, our knowledge of both the fundamental mechanisms controlling rock...
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In: Environmental Research Letters, 2020, vol. 15, no. 10, p. 104070
This paper reviews and analyses the past 20 years of change and variability of European mountain permafrost in response to climate change based on time series of ground temperatures along a south–north transect of deep boreholes from Sierra Nevada in Spain (37°N) to Svalbard (78°N), established between 1998 and 2000 during the EU-funded PACE (Permafrost and Climate in Europe) project. In...
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In: Geoscientific Instrumentation, Methods and Data Systems, 2020, vol. 9, no. 2020-2, p. 317–336
Climate-induced warming increasingly leads to degradation of high-alpine permafrost. In order to develop early warning systems for imminent slope destabilization, knowledge about hydrological flow processes in the subsurface is urgently needed. Due to the fast dynamics associated with slope failures, non- or minimally invasive methods are required for inexpensive and timely characterization...
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