An observationally validated theory of viscous flow dynamics at the ice-shelf calving front

An analytical theory is developed for ice flow velocity in a boundary layer couplet at the calving front. The theory has simple quantitative characteristics that relate ice front velocity to thickness, strain rate and shelf width, matching one set of empirically derived relationships (Alley and othe...

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Published in:Journal of Glaciology
Main Author: Hindmarsh, Richard C.A.
Format: Article in Journal/Newspaper
Language:unknown
Published: International Glaciological Society 2012
Subjects:
Online Access:http://nora.nerc.ac.uk/id/eprint/18240/
http://www.igsoc.org/journal/
id ftnerc:oai:nora.nerc.ac.uk:18240
record_format openpolar
spelling ftnerc:oai:nora.nerc.ac.uk:18240 2023-05-15T16:41:52+02:00 An observationally validated theory of viscous flow dynamics at the ice-shelf calving front Hindmarsh, Richard C.A. 2012 http://nora.nerc.ac.uk/id/eprint/18240/ http://www.igsoc.org/journal/ unknown International Glaciological Society Hindmarsh, Richard C.A. orcid:0000-0003-1633-2416 . 2012 An observationally validated theory of viscous flow dynamics at the ice-shelf calving front. Journal of Glaciology, 58 (208). 375-387. https://doi.org/10.3189/2012JoG11J206 <https://doi.org/10.3189/2012JoG11J206> Glaciology Publication - Article PeerReviewed 2012 ftnerc https://doi.org/10.3189/2012JoG11J206 2023-02-04T19:31:38Z An analytical theory is developed for ice flow velocity in a boundary layer couplet at the calving front. The theory has simple quantitative characteristics that relate ice front velocity to thickness, strain rate and shelf width, matching one set of empirically derived relationships (Alley and others, 2008) and implying that these relationships predict ice velocity rather than calving rate. The two boundary layers are where longitudinal and transverse flow fields change from the interior flow to patterns consistent with the calving-front stress condition. Numerical simulations confirm the analytical theory. The quantitative predictions of the theory have low sensitivity to unmeasured parameters and to shelf plan aspect ratio, while its robustness arises from its dependence on the scale invariance of the governing equations. The theory provides insights into calving, the stability of ice-shelf calving fronts, the stability of the grounding line of laterally resisted ice streams, and also suggests that the calving front is an instructive dynamical analogue to the grounding line. Article in Journal/Newspaper Ice Shelf Journal of Glaciology Natural Environment Research Council: NERC Open Research Archive Journal of Glaciology 58 208 375 387
institution Open Polar
collection Natural Environment Research Council: NERC Open Research Archive
op_collection_id ftnerc
language unknown
topic Glaciology
spellingShingle Glaciology
Hindmarsh, Richard C.A.
An observationally validated theory of viscous flow dynamics at the ice-shelf calving front
topic_facet Glaciology
description An analytical theory is developed for ice flow velocity in a boundary layer couplet at the calving front. The theory has simple quantitative characteristics that relate ice front velocity to thickness, strain rate and shelf width, matching one set of empirically derived relationships (Alley and others, 2008) and implying that these relationships predict ice velocity rather than calving rate. The two boundary layers are where longitudinal and transverse flow fields change from the interior flow to patterns consistent with the calving-front stress condition. Numerical simulations confirm the analytical theory. The quantitative predictions of the theory have low sensitivity to unmeasured parameters and to shelf plan aspect ratio, while its robustness arises from its dependence on the scale invariance of the governing equations. The theory provides insights into calving, the stability of ice-shelf calving fronts, the stability of the grounding line of laterally resisted ice streams, and also suggests that the calving front is an instructive dynamical analogue to the grounding line.
format Article in Journal/Newspaper
author Hindmarsh, Richard C.A.
author_facet Hindmarsh, Richard C.A.
author_sort Hindmarsh, Richard C.A.
title An observationally validated theory of viscous flow dynamics at the ice-shelf calving front
title_short An observationally validated theory of viscous flow dynamics at the ice-shelf calving front
title_full An observationally validated theory of viscous flow dynamics at the ice-shelf calving front
title_fullStr An observationally validated theory of viscous flow dynamics at the ice-shelf calving front
title_full_unstemmed An observationally validated theory of viscous flow dynamics at the ice-shelf calving front
title_sort observationally validated theory of viscous flow dynamics at the ice-shelf calving front
publisher International Glaciological Society
publishDate 2012
url http://nora.nerc.ac.uk/id/eprint/18240/
http://www.igsoc.org/journal/
genre Ice Shelf
Journal of Glaciology
genre_facet Ice Shelf
Journal of Glaciology
op_relation Hindmarsh, Richard C.A. orcid:0000-0003-1633-2416 . 2012 An observationally validated theory of viscous flow dynamics at the ice-shelf calving front. Journal of Glaciology, 58 (208). 375-387. https://doi.org/10.3189/2012JoG11J206 <https://doi.org/10.3189/2012JoG11J206>
op_doi https://doi.org/10.3189/2012JoG11J206
container_title Journal of Glaciology
container_volume 58
container_issue 208
container_start_page 375
op_container_end_page 387
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