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2011
A glacier in equilibrium with the climate is characterized by a given geometry. This geometry results from a balance between snow accumulation, ablation (mainly by melting), and the flow that redistributes the mass accumulated at high elevations toward the lower parts of the glacier. If external forcings (climate) or internal forcings (ice flow) change,
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A glacier in equilibrium with the climate is characterized by a given geometry. This geometry results from a balance between snow accumulation, ablation (mainly by melting), and the flow that redistributes the mass accumulated at high elevations toward the lower parts of the glacier. If external forcings (climate) or internal forcings (ice flow) change,
openaire +2 more sources