A theory of glacier dynamics and instabilities Part 1: Topographically confined glaciers

We present a theoretical framework that integrates the dynamics of glaciers with and without the topographic confinement. This Part 1 paper concerns the former, which may exhibit surge cycles when subjected to thermal switches associated with the bed condition. With the topographic trough setting th...

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Main Author: Ou, Hsien Wang
Format: Article in Journal/Newspaper
Language:English
Published: 2021
Subjects:
Online Access:https://doi.org/10.7916/d8-0xpp-qa06
id ftcolumbiauniv:oai:academiccommons.columbia.edu:10.7916/d8-0xpp-qa06
record_format openpolar
spelling ftcolumbiauniv:oai:academiccommons.columbia.edu:10.7916/d8-0xpp-qa06 2023-05-15T16:21:26+02:00 A theory of glacier dynamics and instabilities Part 1: Topographically confined glaciers Ou, Hsien Wang 2021 https://doi.org/10.7916/d8-0xpp-qa06 English eng https://doi.org/10.7916/d8-0xpp-qa06 Ice--Dynamics Glaciers Glaciers--Mathematical models Glaciology Articles 2021 ftcolumbiauniv https://doi.org/10.7916/d8-0xpp-qa06 2021-12-04T23:21:16Z We present a theoretical framework that integrates the dynamics of glaciers with and without the topographic confinement. This Part 1 paper concerns the former, which may exhibit surge cycles when subjected to thermal switches associated with the bed condition. With the topographic trough setting the glacier width and curbing the lateral drainage of the meltwater, the problem falls under the purview of the undrained plastic bed (UPB) formalism. Employing the UPB, we shall examine the external controls of the glacial behavior and test them against observations. Through our non-dimensionalization scheme, we construct a 2-D regime diagram, which allows a ready prognosis of the glacial properties over the full range of the external conditions, both climate- and size-related. We first discern the boundaries separating the glacial regimes of steadycreep, cyclic-surging and steady-sliding. We then apply the regime diagram to observed glaciers for quantitative comparisons. These include the Svalbard glaciers of both normal and surge types, Northeast Greenland Ice Stream characterized by steady-sliding, and Hudson Strait Ice Stream exhibiting cyclic surges. The quantitative validation of our model containing no free parameters suggests that the thermal switch may unify the dynamics of these diverse glaciers. Article in Journal/Newspaper glacier glacier Greenland Hudson Strait Svalbard Columbia University: Academic Commons Svalbard Greenland Hudson Hudson Strait ENVELOPE(-70.000,-70.000,62.000,62.000)
institution Open Polar
collection Columbia University: Academic Commons
op_collection_id ftcolumbiauniv
language English
topic Ice--Dynamics
Glaciers
Glaciers--Mathematical models
Glaciology
spellingShingle Ice--Dynamics
Glaciers
Glaciers--Mathematical models
Glaciology
Ou, Hsien Wang
A theory of glacier dynamics and instabilities Part 1: Topographically confined glaciers
topic_facet Ice--Dynamics
Glaciers
Glaciers--Mathematical models
Glaciology
description We present a theoretical framework that integrates the dynamics of glaciers with and without the topographic confinement. This Part 1 paper concerns the former, which may exhibit surge cycles when subjected to thermal switches associated with the bed condition. With the topographic trough setting the glacier width and curbing the lateral drainage of the meltwater, the problem falls under the purview of the undrained plastic bed (UPB) formalism. Employing the UPB, we shall examine the external controls of the glacial behavior and test them against observations. Through our non-dimensionalization scheme, we construct a 2-D regime diagram, which allows a ready prognosis of the glacial properties over the full range of the external conditions, both climate- and size-related. We first discern the boundaries separating the glacial regimes of steadycreep, cyclic-surging and steady-sliding. We then apply the regime diagram to observed glaciers for quantitative comparisons. These include the Svalbard glaciers of both normal and surge types, Northeast Greenland Ice Stream characterized by steady-sliding, and Hudson Strait Ice Stream exhibiting cyclic surges. The quantitative validation of our model containing no free parameters suggests that the thermal switch may unify the dynamics of these diverse glaciers.
format Article in Journal/Newspaper
author Ou, Hsien Wang
author_facet Ou, Hsien Wang
author_sort Ou, Hsien Wang
title A theory of glacier dynamics and instabilities Part 1: Topographically confined glaciers
title_short A theory of glacier dynamics and instabilities Part 1: Topographically confined glaciers
title_full A theory of glacier dynamics and instabilities Part 1: Topographically confined glaciers
title_fullStr A theory of glacier dynamics and instabilities Part 1: Topographically confined glaciers
title_full_unstemmed A theory of glacier dynamics and instabilities Part 1: Topographically confined glaciers
title_sort theory of glacier dynamics and instabilities part 1: topographically confined glaciers
publishDate 2021
url https://doi.org/10.7916/d8-0xpp-qa06
long_lat ENVELOPE(-70.000,-70.000,62.000,62.000)
geographic Svalbard
Greenland
Hudson
Hudson Strait
geographic_facet Svalbard
Greenland
Hudson
Hudson Strait
genre glacier
glacier
Greenland
Hudson Strait
Svalbard
genre_facet glacier
glacier
Greenland
Hudson Strait
Svalbard
op_relation https://doi.org/10.7916/d8-0xpp-qa06
op_doi https://doi.org/10.7916/d8-0xpp-qa06
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