Glaciological characteristics in the Dome Fuji region and new assessment for “Oldest Ice”

A key objective in palaeo-climatology is the retrieval of a continuous Antarctic ice-core record dating back 1.5 Ma. The identification of a suitable Antarctic site requires sufficient knowledge of the subglacial landscape beneath the Antarctic Ice Sheet. Here, we present new ice thickness informati...

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Published in:The Cryosphere
Main Authors: Karlsson, Nanna B., Binder, Tobias, Eagles, Graeme, Helm, Veit, Pattyn, Frank, Liefferinge, Brice, Eisen, Olaf
Format: Text
Language:English
Published: 2019
Subjects:
Online Access:https://doi.org/10.5194/tc-12-2413-2018
https://tc.copernicus.org/articles/12/2413/2018/
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spelling ftcopernicus:oai:publications.copernicus.org:tc63475 2023-05-15T13:55:28+02:00 Glaciological characteristics in the Dome Fuji region and new assessment for “Oldest Ice” Karlsson, Nanna B. Binder, Tobias Eagles, Graeme Helm, Veit Pattyn, Frank Liefferinge, Brice Eisen, Olaf 2019-01-08 application/pdf https://doi.org/10.5194/tc-12-2413-2018 https://tc.copernicus.org/articles/12/2413/2018/ eng eng doi:10.5194/tc-12-2413-2018 https://tc.copernicus.org/articles/12/2413/2018/ eISSN: 1994-0424 Text 2019 ftcopernicus https://doi.org/10.5194/tc-12-2413-2018 2020-07-20T16:23:11Z A key objective in palaeo-climatology is the retrieval of a continuous Antarctic ice-core record dating back 1.5 Ma. The identification of a suitable Antarctic site requires sufficient knowledge of the subglacial landscape beneath the Antarctic Ice Sheet. Here, we present new ice thickness information from the Dome Fuji region, East Antarctica, based on airborne radar surveys conducted during the 2014/15 and 2016/17 southern summers. Compared to previous maps of the region, the new dataset shows a more complex landscape with networks of valleys and mountain plateaus. We use the new dataset as input in a thermokinematic model that incorporates uncertainties in geothermal heat flux values in order to improve the predictions of potential ice-core sites. Our results show that especially the region immediately south of Dome Fuji station persists as a good candidate site for obtaining an old ice core. An initial assessment of basal conditions revealed the existence of what appears to be subglacial lakes. Further radar data analysis shows overall high continuity of layer stratigraphy in the region. This indicates that extending the age–depth information from the Dome Fuji ice core to a new ice-core drill site is a viable option. Text Antarc* Antarctic Antarctica East Antarctica ice core Ice Sheet Copernicus Publications: E-Journals Antarctic Dome Fuji ENVELOPE(39.700,39.700,-77.317,-77.317) Dome Fuji Station ENVELOPE(39.703,39.703,-77.317,-77.317) East Antarctica The Antarctic The Cryosphere 12 7 2413 2424
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description A key objective in palaeo-climatology is the retrieval of a continuous Antarctic ice-core record dating back 1.5 Ma. The identification of a suitable Antarctic site requires sufficient knowledge of the subglacial landscape beneath the Antarctic Ice Sheet. Here, we present new ice thickness information from the Dome Fuji region, East Antarctica, based on airborne radar surveys conducted during the 2014/15 and 2016/17 southern summers. Compared to previous maps of the region, the new dataset shows a more complex landscape with networks of valleys and mountain plateaus. We use the new dataset as input in a thermokinematic model that incorporates uncertainties in geothermal heat flux values in order to improve the predictions of potential ice-core sites. Our results show that especially the region immediately south of Dome Fuji station persists as a good candidate site for obtaining an old ice core. An initial assessment of basal conditions revealed the existence of what appears to be subglacial lakes. Further radar data analysis shows overall high continuity of layer stratigraphy in the region. This indicates that extending the age–depth information from the Dome Fuji ice core to a new ice-core drill site is a viable option.
format Text
author Karlsson, Nanna B.
Binder, Tobias
Eagles, Graeme
Helm, Veit
Pattyn, Frank
Liefferinge, Brice
Eisen, Olaf
spellingShingle Karlsson, Nanna B.
Binder, Tobias
Eagles, Graeme
Helm, Veit
Pattyn, Frank
Liefferinge, Brice
Eisen, Olaf
Glaciological characteristics in the Dome Fuji region and new assessment for “Oldest Ice”
author_facet Karlsson, Nanna B.
Binder, Tobias
Eagles, Graeme
Helm, Veit
Pattyn, Frank
Liefferinge, Brice
Eisen, Olaf
author_sort Karlsson, Nanna B.
title Glaciological characteristics in the Dome Fuji region and new assessment for “Oldest Ice”
title_short Glaciological characteristics in the Dome Fuji region and new assessment for “Oldest Ice”
title_full Glaciological characteristics in the Dome Fuji region and new assessment for “Oldest Ice”
title_fullStr Glaciological characteristics in the Dome Fuji region and new assessment for “Oldest Ice”
title_full_unstemmed Glaciological characteristics in the Dome Fuji region and new assessment for “Oldest Ice”
title_sort glaciological characteristics in the dome fuji region and new assessment for “oldest ice”
publishDate 2019
url https://doi.org/10.5194/tc-12-2413-2018
https://tc.copernicus.org/articles/12/2413/2018/
long_lat ENVELOPE(39.700,39.700,-77.317,-77.317)
ENVELOPE(39.703,39.703,-77.317,-77.317)
geographic Antarctic
Dome Fuji
Dome Fuji Station
East Antarctica
The Antarctic
geographic_facet Antarctic
Dome Fuji
Dome Fuji Station
East Antarctica
The Antarctic
genre Antarc*
Antarctic
Antarctica
East Antarctica
ice core
Ice Sheet
genre_facet Antarc*
Antarctic
Antarctica
East Antarctica
ice core
Ice Sheet
op_source eISSN: 1994-0424
op_relation doi:10.5194/tc-12-2413-2018
https://tc.copernicus.org/articles/12/2413/2018/
op_doi https://doi.org/10.5194/tc-12-2413-2018
container_title The Cryosphere
container_volume 12
container_issue 7
container_start_page 2413
op_container_end_page 2424
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