Accurate modelling of glacier flow ...

Recent interest in climatic change and ice .sheet variations points out the need for accurate and numerically stable models of time-dependent ice masses. Little attention has been paid to this topic by the glaciological community, and there is good reason to believe that much of the published litera...

Full description

Bibliographic Details
Main Author: Waddington, Edwin Donald
Format: Text
Language:English
Published: University of British Columbia 2010
Subjects:
Online Access:https://dx.doi.org/10.14288/1.0052458
https://doi.library.ubc.ca/10.14288/1.0052458
id ftdatacite:10.14288/1.0052458
record_format openpolar
spelling ftdatacite:10.14288/1.0052458 2024-04-28T08:24:56+00:00 Accurate modelling of glacier flow ... Waddington, Edwin Donald 2010 https://dx.doi.org/10.14288/1.0052458 https://doi.library.ubc.ca/10.14288/1.0052458 en eng University of British Columbia article-journal Text ScholarlyArticle 2010 ftdatacite https://doi.org/10.14288/1.0052458 2024-04-02T09:36:37Z Recent interest in climatic change and ice .sheet variations points out the need for accurate and numerically stable models of time-dependent ice masses. Little attention has been paid to this topic by the glaciological community, and there is good reason to believe that much of the published literature on numerical modelling of the flow of glaciers and ice sheets is quantitatively incorrect. In particular, the importance of the nonlinear instability has not been widely recognized. The purposes of this thesis are to develop and to verify a new numerical model for glacier flow, compare the model to another widely accepted model, and to demonstrate the model in several glaciologically interesting applications. As in earlier work, the computer model solves the continuity equation together with a flow law for ice. Thickness profiles along flow lines are obtained as a function of time for a temperate ice mass with arbitrary bed topography and mass balance. A set of necessary tests to be satisfied by any numerical ... 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 Recent interest in climatic change and ice .sheet variations points out the need for accurate and numerically stable models of time-dependent ice masses. Little attention has been paid to this topic by the glaciological community, and there is good reason to believe that much of the published literature on numerical modelling of the flow of glaciers and ice sheets is quantitatively incorrect. In particular, the importance of the nonlinear instability has not been widely recognized. The purposes of this thesis are to develop and to verify a new numerical model for glacier flow, compare the model to another widely accepted model, and to demonstrate the model in several glaciologically interesting applications. As in earlier work, the computer model solves the continuity equation together with a flow law for ice. Thickness profiles along flow lines are obtained as a function of time for a temperate ice mass with arbitrary bed topography and mass balance. A set of necessary tests to be satisfied by any numerical ...
format Text
author Waddington, Edwin Donald
spellingShingle Waddington, Edwin Donald
Accurate modelling of glacier flow ...
author_facet Waddington, Edwin Donald
author_sort Waddington, Edwin Donald
title Accurate modelling of glacier flow ...
title_short Accurate modelling of glacier flow ...
title_full Accurate modelling of glacier flow ...
title_fullStr Accurate modelling of glacier flow ...
title_full_unstemmed Accurate modelling of glacier flow ...
title_sort accurate modelling of glacier flow ...
publisher University of British Columbia
publishDate 2010
url https://dx.doi.org/10.14288/1.0052458
https://doi.library.ubc.ca/10.14288/1.0052458
genre Ice Sheet
genre_facet Ice Sheet
op_doi https://doi.org/10.14288/1.0052458
_version_ 1797584933999345664