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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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 |
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Open Polar |
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Copernicus Publications: E-Journals |
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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 |
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12 |
container_issue |
7 |
container_start_page |
2413 |
op_container_end_page |
2424 |
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1766262128442867712 |