In: Scientific Reports, 2020, vol. 10, no. 1, p. 10420
The Mont-Blanc massif, being iconic with its large glaciers and peaks of over 4,000 m, will experience a sharp increase in summer temperatures during the twenty-first century. By 2100, the impact of climate change on the cryosphere and hydrosphere in the Alps is expected to lead to a decrease in annual river discharge. In this work, we modelled the twenty-first century evolution of runoff in...
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In: Geomorphology, 2020, vol. 350, p. 106913
De-glaciating high mountain areas result in new landscapes of bedrock and debris where permafrost can degrade, persist or even newly form in cases, and of new lakes in glacier bed overdeepenings (GBOs) becoming ice-free. These landscapes with new lakes in close neighborhood to over-steepened and perennially frozen slopes are prone to chain reaction processes (e.g. rock-ice avalanches into...
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In: Swiss Journal of Geosciences, 2013, vol. 106, no. 3, p. 469-489
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In: Climatic Change, 2012, vol. 111, no. 2, p. 301-334
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In: International Journal of Earth Sciences, 2001, vol. 90, no. 3, p. 685-702
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In: Environmental Conservation, 1988, vol. 15, no. 1, p. 76-77
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In: Transactions of the Royal Society of Edinburgh: Earth Sciences, 2000, vol. 91, no. 1-2, p. 221-233
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In: Antiquity, 2005, vol. 79, no. 305, p. 725-726
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In: Financial History Review, 2007, vol. 14, no. 1, p. 115-116
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In: Environmental Conservation, 1986, vol. 13, no. 1, p. 80-80
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