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...
Main Authors: | , , , , , , |
---|---|
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 |
id |
doaj-1e7b9ed8a5b842ab82647605d94b0179 |
---|---|
record_format |
Article |
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 |
work_keys_str_mv |
AT ejgowan icesheet10aprogramtoproducepaleoicesheetreconstructionswithminimalassumptions AT ptregoning icesheet10aprogramtoproducepaleoicesheetreconstructionswithminimalassumptions AT apurcell icesheet10aprogramtoproducepaleoicesheetreconstructionswithminimalassumptions AT jlea icesheet10aprogramtoproducepaleoicesheetreconstructionswithminimalassumptions AT ojfransner icesheet10aprogramtoproducepaleoicesheetreconstructionswithminimalassumptions AT rnoormets icesheet10aprogramtoproducepaleoicesheetreconstructionswithminimalassumptions AT jadowdeswell icesheet10aprogramtoproducepaleoicesheetreconstructionswithminimalassumptions |
_version_ |
1725439554456911872 |