Titlebook: Dynamics of Ice Sheets and Glaciers; Ralf Greve,Heinz Blatter Book 2009 Springer-Verlag Berlin Heidelberg 2009 Geophysics.dynamics.flow.gl

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Book 2009f general continuum mechanics, the different initial-boundary-value problems for the flow of ice sheets, ice shelves, ice caps and glaciers are systematically derived. Special emphasis is put on developing hierarchies of approximations for the different systems, and suitable numerical solution techn

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insurgent

‘Anglo-America’ and Atlantic Europeorth America, northern Europe, etc. (see Chapter 1). These ice sheets, with typical thicknesses of several kilometres, impose therefore large, time-dependent loads on the crust of the Earth, to which the body of the Earth as a visco-elastic, multi-layer system reacts with a delayed, essentially vertical displacement.

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Elements of Continuum Mechanics,ce ., and the continuous set of position vectors for all particles of the body is called a . of the body. If . is the actual time, the corresponding configuration is called the ... In addition, we define a .. which refers to a fixed (or initial) time ...

Fester

Glacial Isostasy,orth America, northern Europe, etc. (see Chapter 1). These ice sheets, with typical thicknesses of several kilometres, impose therefore large, time-dependent loads on the crust of the Earth, to which the body of the Earth as a visco-elastic, multi-layer system reacts with a delayed, essentially vertical displacement.

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nepotism