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DEBRIS-COVERED GLACIERS AND ROCK GLACIERS
2014The debris-covered glaciers are observed all over the glaciation regions of the world (Alps, Antarctica, Greenland, Ants, Cascades, Rocky Mountains and ext.). The debris covered glaciers are the formations which occur as a result of the recession of normal glaciers.
GÜRGEN, Gürcan, Çaliskan, Onur
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Inferring Debris Properties on Debris-Covered Glaciers
Debris covers glaciers worldwide and controls sub-debris melt rates by modifying energy transfer from the atmosphere to the ice. Physical properties like thermal conductivity (k) and surface roughness (z0) have been derived from limited local measurements, with models often relying on literature values from a few sites and studies.Vicente Melo Velasco +6 more
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Inferring Debris Properties on Debris-Covered Glaciers: Implications for Glacier Modelling
Debris, ranging from thin surface dust to medial moraines and thick, continuous layers in ablation zones, partially covers glaciers all around the world. By modifying energy transfer from the atmosphere to the ice, the supraglacial debris layer fundamentally controls sub-debris melt rates.Vicente Melo Velasco +5 more
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Hydrology of Debris-Covered Glaciers in High Mountain Asia
Earth-Science Reviews, 2020Evan Stewart Miles +2 more
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