Modelling Laurentide ice stream thermomechanics ...

Ice streams are fast-flow currents which represent a small areal fraction in an ice sheet but account for the majority of ice sheet drainage. Because ice streams are inherently complex and are subgrid in current numerical models, they have not been portrayed in large-scale ice sheet studies. I emplo...

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Main Author: Marshall, Shawn Joseph
Format: Text
Language:English
Published: University of British Columbia 2009
Subjects:
Online Access:https://dx.doi.org/10.14288/1.0053153
https://doi.library.ubc.ca/10.14288/1.0053153
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spelling ftdatacite:10.14288/1.0053153 2024-04-28T08:24:37+00:00 Modelling Laurentide ice stream thermomechanics ... Marshall, Shawn Joseph 2009 https://dx.doi.org/10.14288/1.0053153 https://doi.library.ubc.ca/10.14288/1.0053153 en eng University of British Columbia article-journal Text ScholarlyArticle 2009 ftdatacite https://doi.org/10.14288/1.0053153 2024-04-02T09:40:39Z Ice streams are fast-flow currents which represent a small areal fraction in an ice sheet but account for the majority of ice sheet drainage. Because ice streams are inherently complex and are subgrid in current numerical models, they have not been portrayed in large-scale ice sheet studies. I employ a continuum mixture framework to incorporate ice streams in a three-dimensional thermomechanical model of the Laurentide Ice Sheet. The ice mass is composed of a binary mixture of sheet ice, which flows by viscous creep deformation, and stream ice, which flows by decoupled sliding and/or sediment deformation at the bed. Dynamic and thermal evolutions are solved for each component in the mixture, with coupling rules to govern transfer between flow regimes. These transfers represent the activation, growth, and deactivation of ice streams, manifest by creep exchange and bed exchange of ice. I express the governing equations for mass, momentum, and energy balance in a form suitable for direct incorporation in ... Text Ice Sheet DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
description Ice streams are fast-flow currents which represent a small areal fraction in an ice sheet but account for the majority of ice sheet drainage. Because ice streams are inherently complex and are subgrid in current numerical models, they have not been portrayed in large-scale ice sheet studies. I employ a continuum mixture framework to incorporate ice streams in a three-dimensional thermomechanical model of the Laurentide Ice Sheet. The ice mass is composed of a binary mixture of sheet ice, which flows by viscous creep deformation, and stream ice, which flows by decoupled sliding and/or sediment deformation at the bed. Dynamic and thermal evolutions are solved for each component in the mixture, with coupling rules to govern transfer between flow regimes. These transfers represent the activation, growth, and deactivation of ice streams, manifest by creep exchange and bed exchange of ice. I express the governing equations for mass, momentum, and energy balance in a form suitable for direct incorporation in ...
format Text
author Marshall, Shawn Joseph
spellingShingle Marshall, Shawn Joseph
Modelling Laurentide ice stream thermomechanics ...
author_facet Marshall, Shawn Joseph
author_sort Marshall, Shawn Joseph
title Modelling Laurentide ice stream thermomechanics ...
title_short Modelling Laurentide ice stream thermomechanics ...
title_full Modelling Laurentide ice stream thermomechanics ...
title_fullStr Modelling Laurentide ice stream thermomechanics ...
title_full_unstemmed Modelling Laurentide ice stream thermomechanics ...
title_sort modelling laurentide ice stream thermomechanics ...
publisher University of British Columbia
publishDate 2009
url https://dx.doi.org/10.14288/1.0053153
https://doi.library.ubc.ca/10.14288/1.0053153
genre Ice Sheet
genre_facet Ice Sheet
op_doi https://doi.org/10.14288/1.0053153
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