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• W201127780 abstract "Glaciers and ice sheets gain material through accumulation of snow above the equilibrium line; they lose mass through ablation and meltwater runoff at lower elevations below the equilibrium line, and through iceberg calving where the terminus is in contact with the ocean or proglacial lakes. Additionally, mass may be gained or lost through freezing or melting at the glacier base; but for grounded ice masses, this component of the mass balance is generally small. The objective of modeling glaciers is to develop quantitative models to describe the transfer of mass from the accumulation zone to the ablation region." @default.
• W201127780 created "2016-06-24" @default.
• W201127780 creator A5072364598 @default.
• W201127780 date "2013-01-01" @default.
• W201127780 modified "2023-09-27" @default.
• W201127780 title "8.5 Ice Properties and Glacier Dynamics" @default.
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• W201127780 doi "https://doi.org/10.1016/b978-0-12-374739-6.00194-9" @default.
• W201127780 hasPublicationYear "2013" @default.
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