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 1.2Ma, the recovery of a suitable 1.5 million-year-old ice core is fundamental. The quest for such an Oldest Ice core requires a number of key boundary conditions, of which the poorly known basal geother...

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Main Authors: Van Liefferinge, Brice, Pattyn, Frank, Cavitte, Marie G. P., Karlsson, Nanna B., Young, Duncan A., Sutter, Johannes, Eisen, Olaf
Format: Article in Journal/Newspaper
Language:unknown
Published: Copernicus 2018
Subjects:
Online Access:https://epic.awi.de/id/eprint/47685/
https://epic.awi.de/id/eprint/47685/1/tc-2017-276.pdf
https://hdl.handle.net/10013/epic.4f573247-cf7d-4e94-ab8d-5b094a3b696f
https://hdl.handle.net/
id ftawi:oai:epic.awi.de:47685
record_format openpolar
spelling ftawi:oai:epic.awi.de:47685 2023-05-15T13:45:21+02:00 Promising Oldest Ice sites in East Antarctica based on thermodynamical modelling Van Liefferinge, Brice Pattyn, Frank Cavitte, Marie G. P. Karlsson, Nanna B. Young, Duncan A. Sutter, Johannes Eisen, Olaf 2018-07-26 application/pdf https://epic.awi.de/id/eprint/47685/ https://epic.awi.de/id/eprint/47685/1/tc-2017-276.pdf https://hdl.handle.net/10013/epic.4f573247-cf7d-4e94-ab8d-5b094a3b696f https://hdl.handle.net/ unknown Copernicus https://epic.awi.de/id/eprint/47685/1/tc-2017-276.pdf https://hdl.handle.net/ Van Liefferinge, B. , Pattyn, F. , Cavitte, M. G. P. , Karlsson, N. B. , Young, D. A. , Sutter, J. and Eisen, O. orcid:0000-0002-6380-962X (2018) Promising Oldest Ice sites in East Antarctica based on thermodynamical modelling , The Cryosphere Discussions, pp. 1-22 . doi:10.5194/tc-2017-276 <https://doi.org/10.5194/tc-2017-276> , hdl:10013/epic.4f573247-cf7d-4e94-ab8d-5b094a3b696f info:eu-repo/semantics/openAccess EPIC3The Cryosphere Discussions, Copernicus, pp. 1-22, ISSN: 1994-0440 Article notRev info:eu-repo/semantics/article 2018 ftawi https://doi.org/10.5194/tc-2017-276 2021-12-24T15:44:00Z To resolve the mechanisms behind the major climate reorganisation which occurred between 0.9 and 1.2Ma, the recovery of a suitable 1.5 million-year-old ice core is fundamental. The quest for such 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 1D 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 2Ma, 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 2Ma 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 allows for Oldest Ice. Article in Journal/Newspaper Antarc* Antarctica East Antarctica ice core Ice Sheet The Cryosphere The Cryosphere Discussions Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) Dome Fuji ENVELOPE(39.700,39.700,-77.317,-77.317) East Antarctica
institution Open Polar
collection Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center)
op_collection_id ftawi
language unknown
description To resolve the mechanisms behind the major climate reorganisation which occurred between 0.9 and 1.2Ma, the recovery of a suitable 1.5 million-year-old ice core is fundamental. The quest for such 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 1D 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 2Ma, 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 2Ma 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 allows for Oldest Ice.
format Article in Journal/Newspaper
author Van Liefferinge, Brice
Pattyn, Frank
Cavitte, Marie G. P.
Karlsson, Nanna B.
Young, Duncan A.
Sutter, Johannes
Eisen, Olaf
spellingShingle Van Liefferinge, Brice
Pattyn, Frank
Cavitte, Marie G. P.
Karlsson, Nanna B.
Young, Duncan A.
Sutter, Johannes
Eisen, Olaf
Promising Oldest Ice sites in East Antarctica based on thermodynamical modelling
author_facet Van Liefferinge, Brice
Pattyn, Frank
Cavitte, Marie G. P.
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
publishDate 2018
url https://epic.awi.de/id/eprint/47685/
https://epic.awi.de/id/eprint/47685/1/tc-2017-276.pdf
https://hdl.handle.net/10013/epic.4f573247-cf7d-4e94-ab8d-5b094a3b696f
https://hdl.handle.net/
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
The Cryosphere Discussions
genre_facet Antarc*
Antarctica
East Antarctica
ice core
Ice Sheet
The Cryosphere
The Cryosphere Discussions
op_source EPIC3The Cryosphere Discussions, Copernicus, pp. 1-22, ISSN: 1994-0440
op_relation https://epic.awi.de/id/eprint/47685/1/tc-2017-276.pdf
https://hdl.handle.net/
Van Liefferinge, B. , Pattyn, F. , Cavitte, M. G. P. , Karlsson, N. B. , Young, D. A. , Sutter, J. and Eisen, O. orcid:0000-0002-6380-962X (2018) Promising Oldest Ice sites in East Antarctica based on thermodynamical modelling , The Cryosphere Discussions, pp. 1-22 . doi:10.5194/tc-2017-276 <https://doi.org/10.5194/tc-2017-276> , hdl:10013/epic.4f573247-cf7d-4e94-ab8d-5b094a3b696f
op_rights info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.5194/tc-2017-276
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