Densification rates of snow at polar glaciers
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The densification process of snow at polar glaciers is explained as a pressure sintering phenomenon, and the strain rates of snow densification obtained from density-depth relationships at two polar sites are discussed in terms of pressure sintering parameters. It is found that the power law and diffusional creep mechanisms are important at shallower and deeper depths respectively than the depth of air bubble close-off.
- 国立極地研究所の論文
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関連論文
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