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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The Politico-Economic Dimension is an abstract definition which has many possible realisations (numbers, functions, geometric objects and so on). For our purposes, it is sufficient to consider one of them, namely the geometric object of an . in the three-dimensional, Euclidian, physical space .. Therefore, in our sense a vector a

勾引

Realism, Internationalism, Globalismaterial elements, called .. For any time ., each particle is identified by a position vector x (relative to a prescribed origin .) in the physical space ., 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 c

CURB

Well-Being, Paid Work and Personal Lifels, that is, the water molecules are arranged in layers of hexagonal rings (Fig. 4.1). The plane of such a layer is called the ., which actually consists of two planes shifted slightly (by 0.0923?nm) against each other. The direction perpendicular to the basal planes is the . or ., and the distance

Transfusion

Judith Sixsmith,Margaret Bonehamlow of ice in an ice sheet. Figure 5.1 shows the typical geometry (cross section) of a grounded ice sheet with attached floating ice shelf (the latter will be treated in Chap. 6), as well as its interactions with the atmosphere (snowfall, melting), the lithosphere (geothermal heat flux, isostasy) an

handle

大方一點

Dimitris Ballas,Danny Dorling,Mary Shawilometres in diameter down to small glaciers of a few hundreds of metres in length. Consequently, the scaling given for ice sheets in Chapter 5 [Eqs. (5.5) and (5.102)] is not valid for smaller ice caps and glaciers, and needs to be modified. However, the Froude number (5.7) and Coriolis-force-to-pr

fringe

‘Anglo-America’ and Atlantic Europer only in Antarctica and Greenland, whereas during the Last Glacial Maximum (LGM), 21,000 years ago, extended ice sheets also covered large parts of North America, northern Europe, etc. (see Chapter 1). These ice sheets, with typical thicknesses of several kilometres, impose therefore large, time-de

acrimony

‘Anglo-America’ and Atlantic Europetopics at the forefront of current research. The selection of the topics (induced anisotropy, compressible firn, polythermal glaciers) is strongly influenced by the authors’ own research interests and makes no claim to be complete. Other issues, such as subglacial hydrology, ice stream dynamics or c

Coma704

‘Anglo-America’ and Atlantic EuropeIn agreement with the scope of the series . (AGEM.), it is our intention that this book serves the purposes

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