ICESHEET 1.0: a program to produce paleo-ice sheet reconstructions with minimal assumptions

We describe a program that produces paleo-ice sheet reconstructions using an assumption of steady-state, perfectly plastic ice flow behaviour. It incorporates three input parameters: ice margin, basal shear stress and basal topography. Though it is unlikely that paleo-ice sheets were ever in complet...

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Main Authors: E. J. Gowan, P. Tregoning, A. Purcell, J. Lea, O. J. Fransner, R. Noormets, J. A. Dowdeswell
Format: Article
Language:English
Published: Copernicus Publications 2016-05-01
Series:Geoscientific Model Development
Online Access:http://www.geosci-model-dev.net/9/1673/2016/gmd-9-1673-2016.pdf
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spelling doaj-1e7b9ed8a5b842ab82647605d94b01792020-11-25T00:02:05ZengCopernicus PublicationsGeoscientific Model Development1991-959X1991-96032016-05-01951673168210.5194/gmd-9-1673-2016ICESHEET 1.0: a program to produce paleo-ice sheet reconstructions with minimal assumptionsE. J. Gowan0P. Tregoning1A. Purcell2J. Lea3O. J. Fransner4R. Noormets5J. A. Dowdeswell6Department of Physical Geography, Stockholm University, Stockholm, SwedenResearch School of Earth Science, The Australian National University, Canberra, AustraliaResearch School of Earth Science, The Australian National University, Canberra, AustraliaSchool of Environmental Sciences, University of Liverpool, Liverpool, UKDepartment of Arctic Geology, The University Center in Svalbard (UNIS), Longyearbyen, NorwayDepartment of Arctic Geology, The University Center in Svalbard (UNIS), Longyearbyen, NorwayScott Polar Research Institute, Cambridge, UKWe describe a program that produces paleo-ice sheet reconstructions using an assumption of steady-state, perfectly plastic ice flow behaviour. It incorporates three input parameters: ice margin, basal shear stress and basal topography. Though it is unlikely that paleo-ice sheets were ever in complete steady-state conditions, this method can produce an ice sheet without relying on complicated and unconstrained parameters such as climate and ice dynamics. This makes it advantageous to use in glacial-isostatic adjustment ice sheet modelling, which are often used as input parameters in global climate modelling simulations. We test this program by applying it to the modern Greenland Ice Sheet and Last Glacial Maximum Barents Sea Ice Sheet and demonstrate the optimal parameters that balance computational time and accuracy.http://www.geosci-model-dev.net/9/1673/2016/gmd-9-1673-2016.pdf
collection DOAJ
language English
format Article
sources DOAJ
author E. J. Gowan
P. Tregoning
A. Purcell
J. Lea
O. J. Fransner
R. Noormets
J. A. Dowdeswell
spellingShingle E. J. Gowan
P. Tregoning
A. Purcell
J. Lea
O. J. Fransner
R. Noormets
J. A. Dowdeswell
ICESHEET 1.0: a program to produce paleo-ice sheet reconstructions with minimal assumptions
Geoscientific Model Development
author_facet E. J. Gowan
P. Tregoning
A. Purcell
J. Lea
O. J. Fransner
R. Noormets
J. A. Dowdeswell
author_sort E. J. Gowan
title ICESHEET 1.0: a program to produce paleo-ice sheet reconstructions with minimal assumptions
title_short ICESHEET 1.0: a program to produce paleo-ice sheet reconstructions with minimal assumptions
title_full ICESHEET 1.0: a program to produce paleo-ice sheet reconstructions with minimal assumptions
title_fullStr ICESHEET 1.0: a program to produce paleo-ice sheet reconstructions with minimal assumptions
title_full_unstemmed ICESHEET 1.0: a program to produce paleo-ice sheet reconstructions with minimal assumptions
title_sort icesheet 1.0: a program to produce paleo-ice sheet reconstructions with minimal assumptions
publisher Copernicus Publications
series Geoscientific Model Development
issn 1991-959X
1991-9603
publishDate 2016-05-01
description We describe a program that produces paleo-ice sheet reconstructions using an assumption of steady-state, perfectly plastic ice flow behaviour. It incorporates three input parameters: ice margin, basal shear stress and basal topography. Though it is unlikely that paleo-ice sheets were ever in complete steady-state conditions, this method can produce an ice sheet without relying on complicated and unconstrained parameters such as climate and ice dynamics. This makes it advantageous to use in glacial-isostatic adjustment ice sheet modelling, which are often used as input parameters in global climate modelling simulations. We test this program by applying it to the modern Greenland Ice Sheet and Last Glacial Maximum Barents Sea Ice Sheet and demonstrate the optimal parameters that balance computational time and accuracy.
url http://www.geosci-model-dev.net/9/1673/2016/gmd-9-1673-2016.pdf
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