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Thin and ephemeral snow shapes melt and runoff dynamics in the Peruvian Andes. [PDF]
Fyffe CL +14 more
europepmc +1 more source
SIESTA Project: Svalbard summer 2025 expedition report. [PDF]
Mourot R +9 more
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Peak glacier extinction in the mid-twenty-first century. [PDF]
Van Tricht L +9 more
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Younger Dryas glacier advances in the tropical Andes driven by increased precipitation. [PDF]
Glasser NF +15 more
europepmc +1 more source
Future projections of glacier mass change in High Mountain Asia using GRACE and climatemodel data. [PDF]
Dharpure JK, Howat IM, Patel A.
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Snow avalanche susceptibility, hazard, and exposure assessment in the Western Himalaya using machine learning and numerical modelling. [PDF]
Abhinav A, Sattar A.
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Geological Journal, 2022
Debris‐covered glacier mapping for monitoring glacier fluctuations is necessary to prevent geohazards caused by glaciers. Recently, deep learning‐based methods have been widely utilized for the identification of debris‐covered glaciers.
Ruoshen Lin, Gang Mei, N. Xu
semanticscholar +1 more source
Debris‐covered glacier mapping for monitoring glacier fluctuations is necessary to prevent geohazards caused by glaciers. Recently, deep learning‐based methods have been widely utilized for the identification of debris‐covered glaciers.
Ruoshen Lin, Gang Mei, N. Xu
semanticscholar +1 more source
Evolution of the debris-covered Miage Glacier
2021<p>Glaciers in high-mountain regions typically exhibit a debris cover that moderates their response to climatic change. Here we present an integrated study that integrates long-term observations of debris-covered glacier mass balance, velocity, surface debris evolution and geomorphological changes (such as ponds and ice cliffs) of Miage ...
Anne Stefaniak +5 more
openaire +1 more source
2018
Debris-covered glaciers are characterised by a mantle of rock material, the supraglacial debris, spread over part of the ablation zone. The debris material origins from the catchment above and the bedrock below the glacier and appears at the glacier surface in the ablation zone.
Elisabeth Mayr, Wilfried Hagg
openaire +1 more source
Debris-covered glaciers are characterised by a mantle of rock material, the supraglacial debris, spread over part of the ablation zone. The debris material origins from the catchment above and the bedrock below the glacier and appears at the glacier surface in the ablation zone.
Elisabeth Mayr, Wilfried Hagg
openaire +1 more source

