Tonometry 发表于 2025-3-23 13:42:10

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声明 发表于 2025-3-23 15:15:15

The Glacier Systemtem with input, storage, transfer and output of mass. It is a system in dynamic equilibrium where the mass balance depends on input and output. Input or accumulation includes all those ways in which mass is added to a glacier: solid precipitation, wind-drift snow and avalanching, growth of superimpo

责任 发表于 2025-3-23 21:40:47

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Colonnade 发表于 2025-3-24 00:55:09

Ice Composition and Ice Flow: a General Viewhe standard pressure P; V. is the pore volume when the pores are finally closed off in the firn at temperature T. and air pressure P.. The temperatures are expressed in K (Raynaud and Lebel 1979). This is only true if the transformation of snow into ice occurs in the absence of meltwater, i.e. in th

Modicum 发表于 2025-3-24 03:50:35

The Basal Zone of Ice Caps and Ice Sheetsflux of geothermal heat at the base, the temperature near the surface (usually the temperature at a depth of 10 m to avoid seasonal variations) and the vertical and horizontal components of the velocity at every point in the glacier. The term steady state is used here to describe a distribution of t

可耕种 发表于 2025-3-24 08:08:56

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放弃 发表于 2025-3-24 12:43:47

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irritation 发表于 2025-3-24 18:08:43

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Classify 发表于 2025-3-24 21:42:55

Springer Series in Physical Environmenthttp://image.papertrans.cn/i/image/460702.jpg

Filibuster 发表于 2025-3-25 01:48:10

978-3-642-63497-0Springer-Verlag Berlin Heidelberg 1991
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查看完整版本: Titlebook: Ice Composition and Glacier Dynamics; Roland A. Souchez,Reginald D. Lorrain Book 1991 Springer-Verlag Berlin Heidelberg 1991 Glacier dynam