Basal buoyancy and fast-moving glaciers: in defense of analytic force balance

The geometric approach to force balance advocated by T. Hughes in a series of publications has challenged the analytic approach by implying that the latter does not adequately account for basal buoyancy on ice streams, thereby neglecting the contribution to the gravitational driving force associated...

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Main Author: C. J. van der Veen
Format: Article
Language:English
Published: Copernicus Publications 2016-06-01
Series:The Cryosphere
Online Access:http://www.the-cryosphere.net/10/1331/2016/tc-10-1331-2016.pdf
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author C. J. van der Veen
author_facet C. J. van der Veen
author_sort C. J. van der Veen
collection DOAJ
description The geometric approach to force balance advocated by T. Hughes in a series of publications has challenged the analytic approach by implying that the latter does not adequately account for basal buoyancy on ice streams, thereby neglecting the contribution to the gravitational driving force associated with this basal buoyancy. Application of the geometric approach to Byrd Glacier, Antarctica, yields physically unrealistic results, and it is argued that this is because of a key limiting assumption in the geometric approach. A more traditional analytic treatment of force balance shows that basal buoyancy does not affect the balance of forces on ice streams, except locally perhaps, through bridging effects.
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spelling doaj.art-c2d695babbce42d8aeb2728df9cea46e2022-12-22T01:56:11ZengCopernicus PublicationsThe Cryosphere1994-04161994-04242016-06-011031331133710.5194/tc-10-1331-2016Basal buoyancy and fast-moving glaciers: in defense of analytic force balanceC. J. van der Veen0Department of Geography and Atmospheric Science, University of Kansas, 203 Lindley Hall, 1475 Jayhawk Blvd, Lawrence, KS 66045, USAThe geometric approach to force balance advocated by T. Hughes in a series of publications has challenged the analytic approach by implying that the latter does not adequately account for basal buoyancy on ice streams, thereby neglecting the contribution to the gravitational driving force associated with this basal buoyancy. Application of the geometric approach to Byrd Glacier, Antarctica, yields physically unrealistic results, and it is argued that this is because of a key limiting assumption in the geometric approach. A more traditional analytic treatment of force balance shows that basal buoyancy does not affect the balance of forces on ice streams, except locally perhaps, through bridging effects.http://www.the-cryosphere.net/10/1331/2016/tc-10-1331-2016.pdf
spellingShingle C. J. van der Veen
Basal buoyancy and fast-moving glaciers: in defense of analytic force balance
The Cryosphere
title Basal buoyancy and fast-moving glaciers: in defense of analytic force balance
title_full Basal buoyancy and fast-moving glaciers: in defense of analytic force balance
title_fullStr Basal buoyancy and fast-moving glaciers: in defense of analytic force balance
title_full_unstemmed Basal buoyancy and fast-moving glaciers: in defense of analytic force balance
title_short Basal buoyancy and fast-moving glaciers: in defense of analytic force balance
title_sort basal buoyancy and fast moving glaciers in defense of analytic force balance
url http://www.the-cryosphere.net/10/1331/2016/tc-10-1331-2016.pdf
work_keys_str_mv AT cjvanderveen basalbuoyancyandfastmovingglaciersindefenseofanalyticforcebalance