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  • . The model results show that sublimation varies with drift texture and surface topography. The importance of including field-based data for drift texture, topography and microclimate variation in modelling ice sublimation is highlighted. The results also
  • suggest that stable conditions (no ice loss) at polygon centres are possible with either a 1.9°C decrease in mean annual atmospheric temperature or a 12 per cent increase in mean annual relative humidity.