Titlebook: Ice Composition and Glacier Dynamics; Roland A. Souchez,Reginald D. Lorrain Book 1991 Springer-Verlag Berlin Heidelberg 1991 Glacier dynam

Tonometry

声明

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

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Colonnade

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

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

放弃

irritation

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

Filibuster

978-3-642-63497-0Springer-Verlag Berlin Heidelberg 1991