Evaluation of six geothermal heat flux maps for the Antarctic Lambert-Amery glacial system
Basal thermal conditions play an important role in ice sheet dynamics, and they are sensitive to geothermal heat flux (GHF). Here we estimate the basal thermal conditions, including basal temperature, basal melt rate, and friction heat underneath the Lambert-Amery glacier system in east Antarctica,...
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ftcopernicus:oai:publications.copernicus.org:tcd99225 2023-05-15T13:22:09+02:00 Evaluation of six geothermal heat flux maps for the Antarctic Lambert-Amery glacial system Kang, Haoran Zhao, Liyun Wolovick, Michael Moore, John C. 2021-11-30 application/pdf https://doi.org/10.5194/tc-2021-357 https://tc.copernicus.org/preprints/tc-2021-357/ eng eng doi:10.5194/tc-2021-357 https://tc.copernicus.org/preprints/tc-2021-357/ eISSN: 1994-0424 Text 2021 ftcopernicus https://doi.org/10.5194/tc-2021-357 2021-12-06T17:22:31Z Basal thermal conditions play an important role in ice sheet dynamics, and they are sensitive to geothermal heat flux (GHF). Here we estimate the basal thermal conditions, including basal temperature, basal melt rate, and friction heat underneath the Lambert-Amery glacier system in east Antarctica, using a combination of a forward model and an inversion from a 3D ice flow model. We assess the sensitivity and uncertainty of basal thermal conditions using six different GHFs. We evaluate the modelled results using all available observed subglacial lakes. There are very large differences in modelled spatial pattern of temperate basal conditions using the different GHFs. The two most-recent GHF fields inverted from aerial geomagnetic observations have higher values of GHF in the region, produce a larger warm-based area, and match the observed subglacial lakes better than the other GHFs. The fast flowing glacier region has a lower modelled basal friction coefficient, faster basal velocity, with higher basal frictional heating in the range of 50–2000 mW m −2 than the base under slower flowing glaciated areas. The modelled basal melt rate reaches ten to hundreds of mm per year locally in Lambert, Lepekhin and Kronshtadtskiy glaciers feeding the Amery ice shelf, and ranges from 0–5 mm yr −1 on the temperate base of the vast inland region. Text Amery Ice Shelf Antarc* Antarctic Antarctica East Antarctica Ice Sheet Ice Shelf Copernicus Publications: E-Journals Antarctic The Antarctic East Antarctica Amery ENVELOPE(-94.063,-94.063,56.565,56.565) Amery Ice Shelf ENVELOPE(71.000,71.000,-69.750,-69.750) |
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Open Polar |
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Copernicus Publications: E-Journals |
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ftcopernicus |
language |
English |
description |
Basal thermal conditions play an important role in ice sheet dynamics, and they are sensitive to geothermal heat flux (GHF). Here we estimate the basal thermal conditions, including basal temperature, basal melt rate, and friction heat underneath the Lambert-Amery glacier system in east Antarctica, using a combination of a forward model and an inversion from a 3D ice flow model. We assess the sensitivity and uncertainty of basal thermal conditions using six different GHFs. We evaluate the modelled results using all available observed subglacial lakes. There are very large differences in modelled spatial pattern of temperate basal conditions using the different GHFs. The two most-recent GHF fields inverted from aerial geomagnetic observations have higher values of GHF in the region, produce a larger warm-based area, and match the observed subglacial lakes better than the other GHFs. The fast flowing glacier region has a lower modelled basal friction coefficient, faster basal velocity, with higher basal frictional heating in the range of 50–2000 mW m −2 than the base under slower flowing glaciated areas. The modelled basal melt rate reaches ten to hundreds of mm per year locally in Lambert, Lepekhin and Kronshtadtskiy glaciers feeding the Amery ice shelf, and ranges from 0–5 mm yr −1 on the temperate base of the vast inland region. |
format |
Text |
author |
Kang, Haoran Zhao, Liyun Wolovick, Michael Moore, John C. |
spellingShingle |
Kang, Haoran Zhao, Liyun Wolovick, Michael Moore, John C. Evaluation of six geothermal heat flux maps for the Antarctic Lambert-Amery glacial system |
author_facet |
Kang, Haoran Zhao, Liyun Wolovick, Michael Moore, John C. |
author_sort |
Kang, Haoran |
title |
Evaluation of six geothermal heat flux maps for the Antarctic Lambert-Amery glacial system |
title_short |
Evaluation of six geothermal heat flux maps for the Antarctic Lambert-Amery glacial system |
title_full |
Evaluation of six geothermal heat flux maps for the Antarctic Lambert-Amery glacial system |
title_fullStr |
Evaluation of six geothermal heat flux maps for the Antarctic Lambert-Amery glacial system |
title_full_unstemmed |
Evaluation of six geothermal heat flux maps for the Antarctic Lambert-Amery glacial system |
title_sort |
evaluation of six geothermal heat flux maps for the antarctic lambert-amery glacial system |
publishDate |
2021 |
url |
https://doi.org/10.5194/tc-2021-357 https://tc.copernicus.org/preprints/tc-2021-357/ |
long_lat |
ENVELOPE(-94.063,-94.063,56.565,56.565) ENVELOPE(71.000,71.000,-69.750,-69.750) |
geographic |
Antarctic The Antarctic East Antarctica Amery Amery Ice Shelf |
geographic_facet |
Antarctic The Antarctic East Antarctica Amery Amery Ice Shelf |
genre |
Amery Ice Shelf Antarc* Antarctic Antarctica East Antarctica Ice Sheet Ice Shelf |
genre_facet |
Amery Ice Shelf Antarc* Antarctic Antarctica East Antarctica Ice Sheet Ice Shelf |
op_source |
eISSN: 1994-0424 |
op_relation |
doi:10.5194/tc-2021-357 https://tc.copernicus.org/preprints/tc-2021-357/ |
op_doi |
https://doi.org/10.5194/tc-2021-357 |
_version_ |
1766363475372670976 |