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Geophysics
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Glacial isostatic adjustment (GIA) is the Earth's response to glacial-induced load variations on its surface. This phenomenon can today be observed in
North America and Fennoscandia. Different observables
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accurate predictions of the gravity change are important for e.g. reductions of geodetic observations to a reference epoch. During the last decade
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contribute different and complemental information on the phenomenon. Knowledge of the gravitational component is important for understanding the underlying geodynamical processes. Further
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efforts to observe the surface gravity change in Fennoscandia have been intensified and the observational accuracy successively improved. This offers new possibilities at the same time as it puts new demands on modelling. The purpose of this thesis is to study some aspects of the modelling of GIA-induced gravity change
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for example
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relative sea level change and disturbances in the gravity field
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such as vertical and horizontal deformation of the crust
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