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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Online Access: | http://hdl.handle.net/2078.1/257961 https://doi.org/10.5194/tc-12-2773-2018 |
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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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1798835189927903232 |