Improving models of earth's response to ice and ocean loading changes

Patterns of past, present, and future sea level vary spatially, depending on how the solid Earth responds to the changing distribution of ice and ocean mass, known as glacial isostatic adjustment (GIA). Accurate interpretation of observational constraints on GIA requires dialogue between field scien...

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Bibliographic Details
Published in:Eos, Transactions American Geophysical Union
Main Authors: King, MA, Milne, G, Wiens, D
Format: Text
Language:English
Published: American Geophysical Union 2013
Subjects:
Earth Sciences
Geology
Marine Geoscience
Ice Sheet
Online Access:https://doi.org/10.1002/2013EO400007
http://ecite.utas.edu.au/116716
Description
Summary:Patterns of past, present, and future sea level vary spatially, depending on how the solid Earth responds to the changing distribution of ice and ocean mass, known as glacial isostatic adjustment (GIA). Accurate interpretation of observational constraints on GIA requires dialogue between field scientists and researchers who reconstruct ice sheet geometries, infer Earth structure and rheology, and model the solid Earth response to loading.

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