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Titlebook: Ice Sheets and Climate; J. Oerlemans,C. J. Veen Book 1984 D. Reidel Publishing Company, Dordrecht, Holland 1984 Albedo.Ice Age.Ice shelf.P

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s with tumor-associated leukocytes such as macrophages. Indeed, regardless of cell or tissue origin, when cancer cells in the original in situ tumor transform to malignant, invasive cells, they generally become aneuploid and begin to express molecules and traits characteristic of activated macrophag
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Modelling of Ice Flow,s a long way, at least if one desires to go step by step through all required simplifications. A climate modeler wishing to design a dynamical system that describes the response of an ice sheet to changes in environmental conditions may follow another route: by looking carefully at proxy data on the
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Numerical Ice-Sheet Models,ossible will be discussed in chapter 6. In most cases numerical methods have to be used, particularly when we are not only interested in steady states, but also want to compute the transient behaviour of an ice sheet.
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Bedrock Adjustment,alues of more than 4500 m with a mean value of about 2000 m. So a considerable pressure is exerted on the underlying bedrock, which will deflect to restore the equilibrium of forces. In some ice—sheet models the effect of ice thickness on bedrock topography is incorporated by assuming local,isostati
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More About Environmental Conditions,simple function of elevation with respect to the snow line, which itself has been assumed to be a linear function of position. In the first sections of this chapter we will discuss in more detail the basis of such approximations, and see that depending on local conditions a more sophisticated parame
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The Glacial Cycles of the Pleistocene,t of this book to detail in depth with the geological methods that led to the documentation of the ice.ages as we know it now, we will spend a few pages on how ideas about the ‘glacial theory’ evolved, and on what type of material is most useful in the search for an explanation of the glacial cycles
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