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  • , particularly the redistribution of snow by avalanches and wind on soil temperature and the development of permafrost. The results of the study are based on a comparative approach of surveys within and outside the permafrost body at Flüela Pass. A theoretical
  • 2004
  • Rock-face near-surface temperatures have been measured over one year at 14 locations between 2500 and 4500 m a.s.l. in the Alps. These data were used to further develop and verify an energy-balance model that simulates daily surface temperatures
  • 2004