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Linear modelling of glacier length fluctuations
Geografiska Annaler: Series A, Physical Geography, 2012In this contribution a linear first-order differential equation is used to model glacier length fluctuations. This equation has two parameters describing the physical characteristics of a glacier: the climate sensitivity, expressing how the equilibrium glacier length depends on the climatic state, and the response time, indicating how fast a glacier ...
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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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Linear modeling of glacier fluctuations
Geografiska Annaler, Series A: Physical Geography, 2012In this contribution a linear first-order differential equation is used to model glacier length fluctuations. This equation has two parameters describing the physical characteristics of a glacier: the climate sensitivity, expressing how the equilibrium glacier length depends on the climatic state, and the response time, indicating how fast a glacier ...
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Glacier Modeling and the Climate of Patagonia during the Last Glacial Maximum
Quaternary Research, 1994N. Hulton +3 more
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