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Contribution to the modelling of postglacial gravity change in Fennoscandia
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On modelling of postglacial gravity change
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Effects on gravity from non-tidal sea level variations in the Baltic Sea
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Modelling of the GIA-induced surface gravity change over Fennoscandia
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Modelling of the GIA-induced surface gravity change over Fennoscandia
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The relation between gravity rate of change and vertical displacement in previou...
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Postglacial gravity change in Fennoscandia – three decades of repeated absolute...
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Postglacial gravity change in Fennoscandia—three decades of repeated absolute gr...
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Postglacial gravity change in Fennoscandia—three decades of repeated absolute gr...
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Postglacial gravity change in Fennoscandia – three decades of repeated absolute...
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Postglacial gravity change in Fennoscandia—three decades of repeated absolute gr...
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Postglacial gravity change in Fennoscandia - three decades of repeated absolute...
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Postglacial gravity change in Fennoscandia – three decades of repeated absolute...
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Related Subjects
Geophysics
Europe
Dynamics of lithosphere and mantle
Geodetic instrumentation
Reference systems
Time variable gravity
Glacial Isostatic Adjustment
Baltic Sea
Dewey Decimal Classification500 | Naturwissenschaften550 | Geowissenschaften
Earth and Related Environmental Sciences
Earth-Surface Processes
Geodesy and gravity
Glacial isostatic adjustment (GIA) is the Earth's response to glacial-induced load variations on its surface. This phenomenon can today be observed in
Green's function for gravity
Newtonian effect at height
Non-tidal ocean loading
North America and Fennoscandia. Different observables
Rate of change of gravity
accurate predictions of the gravity change are important for e.g. reductions of geodetic observations to a reference epoch. During the last decade
contribute different and complemental information on the phenomenon. Knowledge of the gravitational component is important for understanding the underlying geodynamical processes. Further
ddc:550
dynamics of lithosphere and mantle
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
for example
geodesy and tides
geodetic instrumentation
gravity
gravity change
postglacial rebound
reference systems
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