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On the influence of Greenland outlet glacier bed topography on results from dynamic ice-sheet models

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Please use this identifier to cite or link to this item:http://hdl.handle.net/2115/52825

Title: On the influence of Greenland outlet glacier bed topography on results from dynamic ice-sheet models
Authors: Herzfeld, Ute C. Browse this author
Fastook, James Browse this author
Greve, Ralf Browse this author →KAKEN DB
McDonald, Brian Browse this author
Wallin, Bruce F. Browse this author
Chen, Phillip A. Browse this author
Issue Date: Nov-2012
Publisher: International Glaciological Society
Journal Title: Annals of Glaciology
Volume: 53
Issue: 60
Start Page: 281
End Page: 293
Publisher DOI: 10.3189/2012AoG60A061
Abstract: Prediction of future changes in dynamics of the Earth's ice sheets, mass loss and resultant contribution to sea-level rise are the main objectives of ice-sheet modeling. Mass transfer from ice sheet to ocean is, in large part, through outlet glaciers. Subglacial topography plays an important role in ice dynamics; however, trough systems have not been included in bed digital elevation models (DEMS) used in modeling, because their size is close to the model resolution. Using recently collected CReSIS MCoRDs data of subglacial topography and an algorithm that allows topographically and morphologically correct integration of troughs and trough systems at anymodeling scale (5 kmresolution for SeaRISE), an improved Greenland bed DEM was developed that includes Jakobshavn Isbræ, Helheim, Kangerdlussuaq and Petermann glaciers (JakHelKanPet DEM). Contrasting the different responses of two Greenland ice-sheet models (UMISM and SICOPOLIS) to the more accurately represented bed shows significant differences in modeled surface velocity, basal water production and ice thickness. Consequently, modeled ice volumes for the Greenland ice sheet are significantly smaller using the JakHelKanPet DEM, and volume losses larger. More generally, the study demonstrates the role of spatial modeling of data specifically as input for dynamic ice-sheet models in assessments of future sea-level rise.
Rights: © 2012 International Glaciological Society
Relation: http://www.igsoc.org/annals/
Type: article
URI: http://hdl.handle.net/2115/52825
Appears in Collections:低温科学研究所 (Institute of Low Temperature Science) > 雑誌発表論文等 (Peer-reviewed Journal Articles, etc)

Submitter: Greve Ralf

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