File(s) under permanent embargo
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 scientists and researchers who reconstruct ice sheet geometries, infer Earth structure and rheology, and model the solid Earth response to loading.
History
Publication title
Eos: Transactions, American Geophysical UnionVolume
94Issue
40Pagination
353ISSN
0096-3941Department/School
School of Geography, Planning and Spatial SciencesPublisher
American Geophysical UnionPlace of publication
Washington, DC 20009 United StatesRepository Status
- Restricted