Promising Oldest Ice sites in East Antarctica based on thermodynamical modelling

To resolve the mechanisms behind the major climate reorganisation, which occurred between 0.9 and 1.2 Ma, the recovery of a suitable 1.5 million-year-old ice core is fundamental. The quest for an Oldest Ice core requires a number of key boundary conditions, of which the poorly known basal geotherm...

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Published in:The Cryosphere
Main Authors: Van Liefferinge, Brice, Pattyn, Frank, Cavitte, Marie, Karlsson, Nanna B., Young, Duncan A., Sutter, Johannes, Eisen, Olaf
Other Authors: UCL - SST/ELI/ELIC - Earth & Climate
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus GmbH 2018
Subjects:
Online Access:http://hdl.handle.net/2078.1/257961
https://doi.org/10.5194/tc-12-2773-2018
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spelling ftunistlouisbrus:oai:dial.uclouvain.be:boreal:257961 2024-05-12T07:55:24+00:00 Promising Oldest Ice sites in East Antarctica based on thermodynamical modelling Van Liefferinge, Brice Pattyn, Frank Cavitte, Marie Karlsson, Nanna B. Young, Duncan A. Sutter, Johannes Eisen, Olaf UCL - SST/ELI/ELIC - Earth & Climate 2018 http://hdl.handle.net/2078.1/257961 https://doi.org/10.5194/tc-12-2773-2018 eng eng Copernicus GmbH boreal:257961 http://hdl.handle.net/2078.1/257961 doi:10.5194/tc-12-2773-2018 urn:EISSN:1994-0424 info:eu-repo/semantics/openAccess The Cryosphere, Vol. 12, no.8, p. 2773-2787 (2018) Earth-Surface Processes Water Science and Technology info:eu-repo/semantics/article 2018 ftunistlouisbrus https://doi.org/10.5194/tc-12-2773-2018 2024-04-18T17:14:05Z To resolve the mechanisms behind the major climate reorganisation, which occurred between 0.9 and 1.2 Ma, the recovery of a suitable 1.5 million-year-old ice core is fundamental. The quest for an Oldest Ice core requires a number of key boundary conditions, of which the poorly known basal geothermal heat flux (GHF) is lacking. We use a transient thermodynamical 1-D vertical model that solves for the rate of change of temperature in the vertical, with surface temperature and modelled GHF as boundary conditions. For each point on the ice sheet, the model is forced with variations in atmospheric conditions over the last 2 Ma and modelled ice-thickness variations. The process is repeated for a range of GHF values to determine the value of GHF that marks the limit between frozen and melting conditions over the whole ice sheet, taking into account 2 Ma of climate history. These threshold values of GHF are statistically compared to existing GHF data sets. The new probabilistic GHF fields obtained for the ice sheet thus provide the missing boundary conditions in the search for Oldest Ice. High spatial resolution radar data are examined locally in the Dome Fuji and Dome C regions, as these represent the ice core community's primary drilling sites. GHF, bedrock variability, ice thickness and other essential criteria combined highlight a dozen major potential Oldest Ice sites in the vicinity of Dome Fuji and Dome C, where GHF could allow for Oldest Ice. Article in Journal/Newspaper Antarc* Antarctica East Antarctica ice core Ice Sheet The Cryosphere DIAL@USL-B (Université Saint-Louis, Bruxelles) Dome Fuji ENVELOPE(39.700,39.700,-77.317,-77.317) East Antarctica The Cryosphere 12 8 2773 2787
institution Open Polar
collection DIAL@USL-B (Université Saint-Louis, Bruxelles)
op_collection_id ftunistlouisbrus
language English
topic Earth-Surface Processes
Water Science and Technology
spellingShingle Earth-Surface Processes
Water Science and Technology
Van Liefferinge, Brice
Pattyn, Frank
Cavitte, Marie
Karlsson, Nanna B.
Young, Duncan A.
Sutter, Johannes
Eisen, Olaf
Promising Oldest Ice sites in East Antarctica based on thermodynamical modelling
topic_facet Earth-Surface Processes
Water Science and Technology
description To resolve the mechanisms behind the major climate reorganisation, which occurred between 0.9 and 1.2 Ma, the recovery of a suitable 1.5 million-year-old ice core is fundamental. The quest for an Oldest Ice core requires a number of key boundary conditions, of which the poorly known basal geothermal heat flux (GHF) is lacking. We use a transient thermodynamical 1-D vertical model that solves for the rate of change of temperature in the vertical, with surface temperature and modelled GHF as boundary conditions. For each point on the ice sheet, the model is forced with variations in atmospheric conditions over the last 2 Ma and modelled ice-thickness variations. The process is repeated for a range of GHF values to determine the value of GHF that marks the limit between frozen and melting conditions over the whole ice sheet, taking into account 2 Ma of climate history. These threshold values of GHF are statistically compared to existing GHF data sets. The new probabilistic GHF fields obtained for the ice sheet thus provide the missing boundary conditions in the search for Oldest Ice. High spatial resolution radar data are examined locally in the Dome Fuji and Dome C regions, as these represent the ice core community's primary drilling sites. GHF, bedrock variability, ice thickness and other essential criteria combined highlight a dozen major potential Oldest Ice sites in the vicinity of Dome Fuji and Dome C, where GHF could allow for Oldest Ice.
author2 UCL - SST/ELI/ELIC - Earth & Climate
format Article in Journal/Newspaper
author Van Liefferinge, Brice
Pattyn, Frank
Cavitte, Marie
Karlsson, Nanna B.
Young, Duncan A.
Sutter, Johannes
Eisen, Olaf
author_facet Van Liefferinge, Brice
Pattyn, Frank
Cavitte, Marie
Karlsson, Nanna B.
Young, Duncan A.
Sutter, Johannes
Eisen, Olaf
author_sort Van Liefferinge, Brice
title Promising Oldest Ice sites in East Antarctica based on thermodynamical modelling
title_short Promising Oldest Ice sites in East Antarctica based on thermodynamical modelling
title_full Promising Oldest Ice sites in East Antarctica based on thermodynamical modelling
title_fullStr Promising Oldest Ice sites in East Antarctica based on thermodynamical modelling
title_full_unstemmed Promising Oldest Ice sites in East Antarctica based on thermodynamical modelling
title_sort promising oldest ice sites in east antarctica based on thermodynamical modelling
publisher Copernicus GmbH
publishDate 2018
url http://hdl.handle.net/2078.1/257961
https://doi.org/10.5194/tc-12-2773-2018
long_lat ENVELOPE(39.700,39.700,-77.317,-77.317)
geographic Dome Fuji
East Antarctica
geographic_facet Dome Fuji
East Antarctica
genre Antarc*
Antarctica
East Antarctica
ice core
Ice Sheet
The Cryosphere
genre_facet Antarc*
Antarctica
East Antarctica
ice core
Ice Sheet
The Cryosphere
op_source The Cryosphere, Vol. 12, no.8, p. 2773-2787 (2018)
op_relation boreal:257961
http://hdl.handle.net/2078.1/257961
doi:10.5194/tc-12-2773-2018
urn:EISSN:1994-0424
op_rights info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.5194/tc-12-2773-2018
container_title The Cryosphere
container_volume 12
container_issue 8
container_start_page 2773
op_container_end_page 2787
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