An ice-shelf model test based on the Ross ice shelf

A standard numerical experiment featuring the Ross Ice Shelf, Antarctica, is presented as a test package for the development and intercomparison of ice-shelf models. The emphasis of this package is solution of stress-equilibrium equations for an ice-shelf velocity consistent with present observation...

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Main Authors: MacAyeal, D. R., Rommelaere, V., Huybrechts, P., Hulbe, Christina L., Determann, J., Ritz, C.
Format: Text
Language:unknown
Published: PDXScholar 1996
Subjects:
Online Access:https://pdxscholar.library.pdx.edu/geology_fac/32
https://pdxscholar.library.pdx.edu/cgi/viewcontent.cgi?article=1031&context=geology_fac
id ftportlandstate:oai:pdxscholar.library.pdx.edu:geology_fac-1031
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spelling ftportlandstate:oai:pdxscholar.library.pdx.edu:geology_fac-1031 2023-05-15T13:58:46+02:00 An ice-shelf model test based on the Ross ice shelf MacAyeal, D. R. Rommelaere, V. Huybrechts, P. Hulbe, Christina L. Determann, J. Ritz, C. 1996-01-01T08:00:00Z application/pdf https://pdxscholar.library.pdx.edu/geology_fac/32 https://pdxscholar.library.pdx.edu/cgi/viewcontent.cgi?article=1031&context=geology_fac unknown PDXScholar https://pdxscholar.library.pdx.edu/geology_fac/32 https://pdxscholar.library.pdx.edu/cgi/viewcontent.cgi?article=1031&context=geology_fac Geology Faculty Publications and Presentations Ice sheets -- Antarctica Glaciers -- Antarctica Ice shelves -- Antarctica Glaciers -- Antarctica -- Ross Ice Shelf Geology text 1996 ftportlandstate 2022-01-09T19:24:25Z A standard numerical experiment featuring the Ross Ice Shelf, Antarctica, is presented as a test package for the development and intercomparison of ice-shelf models. The emphasis of this package is solution of stress-equilibrium equations for an ice-shelf velocity consistent with present observations. As a demonstration, we compare five independently developed ice-shelf models based on finite-difference and finite-element methods. Our results suggest that there is little difference between finite-element and finite-difference methods in capturing the basic, large-scale flow features of the ice shelf. We additionally show that the fit between model and observed velocity depends strongly on the ice-shelf temperature field for which there is presently little observational control. The main differences between model results are due to the equations being solved, the boundary conditions at the ice front and the discretization method (finite element vs. finite difference) Text Antarc* Antarctica Ice Shelf Ice Shelves Ross Ice Shelf Portland State University: PDXScholar Ross Ice Shelf
institution Open Polar
collection Portland State University: PDXScholar
op_collection_id ftportlandstate
language unknown
topic Ice sheets -- Antarctica
Glaciers -- Antarctica
Ice shelves -- Antarctica
Glaciers -- Antarctica -- Ross Ice Shelf
Geology
spellingShingle Ice sheets -- Antarctica
Glaciers -- Antarctica
Ice shelves -- Antarctica
Glaciers -- Antarctica -- Ross Ice Shelf
Geology
MacAyeal, D. R.
Rommelaere, V.
Huybrechts, P.
Hulbe, Christina L.
Determann, J.
Ritz, C.
An ice-shelf model test based on the Ross ice shelf
topic_facet Ice sheets -- Antarctica
Glaciers -- Antarctica
Ice shelves -- Antarctica
Glaciers -- Antarctica -- Ross Ice Shelf
Geology
description A standard numerical experiment featuring the Ross Ice Shelf, Antarctica, is presented as a test package for the development and intercomparison of ice-shelf models. The emphasis of this package is solution of stress-equilibrium equations for an ice-shelf velocity consistent with present observations. As a demonstration, we compare five independently developed ice-shelf models based on finite-difference and finite-element methods. Our results suggest that there is little difference between finite-element and finite-difference methods in capturing the basic, large-scale flow features of the ice shelf. We additionally show that the fit between model and observed velocity depends strongly on the ice-shelf temperature field for which there is presently little observational control. The main differences between model results are due to the equations being solved, the boundary conditions at the ice front and the discretization method (finite element vs. finite difference)
format Text
author MacAyeal, D. R.
Rommelaere, V.
Huybrechts, P.
Hulbe, Christina L.
Determann, J.
Ritz, C.
author_facet MacAyeal, D. R.
Rommelaere, V.
Huybrechts, P.
Hulbe, Christina L.
Determann, J.
Ritz, C.
author_sort MacAyeal, D. R.
title An ice-shelf model test based on the Ross ice shelf
title_short An ice-shelf model test based on the Ross ice shelf
title_full An ice-shelf model test based on the Ross ice shelf
title_fullStr An ice-shelf model test based on the Ross ice shelf
title_full_unstemmed An ice-shelf model test based on the Ross ice shelf
title_sort ice-shelf model test based on the ross ice shelf
publisher PDXScholar
publishDate 1996
url https://pdxscholar.library.pdx.edu/geology_fac/32
https://pdxscholar.library.pdx.edu/cgi/viewcontent.cgi?article=1031&context=geology_fac
geographic Ross Ice Shelf
geographic_facet Ross Ice Shelf
genre Antarc*
Antarctica
Ice Shelf
Ice Shelves
Ross Ice Shelf
genre_facet Antarc*
Antarctica
Ice Shelf
Ice Shelves
Ross Ice Shelf
op_source Geology Faculty Publications and Presentations
op_relation https://pdxscholar.library.pdx.edu/geology_fac/32
https://pdxscholar.library.pdx.edu/cgi/viewcontent.cgi?article=1031&context=geology_fac
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