The symmetry group of the CAFFE model

A new ice-sheet flow model called CAFFE (Continuum-mechanical Anisotropic Flow model based on an anisotropic Flow Enhancement factor) has recently become a source of considerable controversy within the glaciological community. Its main proponents (Placidi, Greve and Seddik) defend the thesis that th...

Full description

Bibliographic Details
Published in:Journal of Glaciology
Main Author: Faria, Sergio H.
Format: Article in Journal/Newspaper
Language:unknown
Published: Int Glaciol Soc 2008
Subjects:
Ice Sheet
Online Access:https://resolver.sub.uni-goettingen.de/purl?gro-2/55479
https://doi.org/10.3189/002214308786570935
id ftsubgoettingen:oai:publications.goettingen-research-online.de:2/55479
record_format openpolar
spelling ftsubgoettingen:oai:publications.goettingen-research-online.de:2/55479 2023-07-30T04:04:11+02:00 The symmetry group of the CAFFE model Faria, Sergio H. 2008 https://resolver.sub.uni-goettingen.de/purl?gro-2/55479 https://doi.org/10.3189/002214308786570935 unknown Int Glaciol Soc 0022-1430 https://resolver.sub.uni-goettingen.de/purl?gro-2/55479 doi:10.3189/002214308786570935 000261076300007 journal_article published yes 2008 ftsubgoettingen https://doi.org/10.3189/002214308786570935 2023-07-16T22:13:24Z A new ice-sheet flow model called CAFFE (Continuum-mechanical Anisotropic Flow model based on an anisotropic Flow Enhancement factor) has recently become a source of considerable controversy within the glaciological community. Its main proponents (Placidi, Greve and Seddik) defend the thesis that this model can describe the effect of induced anisotropy on ice-sheet flow, while others assert that the CAFFE model is merely an isotropic model. Here I resolve this dispute by rigorously deriving the symmetry group of the CAFFE model. Article in Journal/Newspaper Ice Sheet Georg-August-Universität Göttingen: GoeScholar Journal of Glaciology 54 187 643 645
institution Open Polar
collection Georg-August-Universität Göttingen: GoeScholar
op_collection_id ftsubgoettingen
language unknown
description A new ice-sheet flow model called CAFFE (Continuum-mechanical Anisotropic Flow model based on an anisotropic Flow Enhancement factor) has recently become a source of considerable controversy within the glaciological community. Its main proponents (Placidi, Greve and Seddik) defend the thesis that this model can describe the effect of induced anisotropy on ice-sheet flow, while others assert that the CAFFE model is merely an isotropic model. Here I resolve this dispute by rigorously deriving the symmetry group of the CAFFE model.
format Article in Journal/Newspaper
author Faria, Sergio H.
spellingShingle Faria, Sergio H.
The symmetry group of the CAFFE model
author_facet Faria, Sergio H.
author_sort Faria, Sergio H.
title The symmetry group of the CAFFE model
title_short The symmetry group of the CAFFE model
title_full The symmetry group of the CAFFE model
title_fullStr The symmetry group of the CAFFE model
title_full_unstemmed The symmetry group of the CAFFE model
title_sort symmetry group of the caffe model
publisher Int Glaciol Soc
publishDate 2008
url https://resolver.sub.uni-goettingen.de/purl?gro-2/55479
https://doi.org/10.3189/002214308786570935
genre Ice Sheet
genre_facet Ice Sheet
op_relation 0022-1430
https://resolver.sub.uni-goettingen.de/purl?gro-2/55479
doi:10.3189/002214308786570935
000261076300007
op_doi https://doi.org/10.3189/002214308786570935
container_title Journal of Glaciology
container_volume 54
container_issue 187
container_start_page 643
op_container_end_page 645
_version_ 1772815419807105024

Similar Items