Ice flow modelling at EPICA Dome C and Dome Fuji, East Antarctica
International audience 1-D ice flow models are used to construct the age scales at the Dome C and Dome Fuji drilling sites (East Antarctica). The poorly constrained glaciological parameters at each site are recovered by fitting independent age markers identified on each core. We reconstruct past acc...
Main Authors: | , , , , , , , , , , , , , , , |
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Other Authors: | , , , , , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
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HAL CCSD
2007
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Subjects: | |
Online Access: | https://hal.science/hal-00330720 https://hal.science/hal-00330720/document https://hal.science/hal-00330720/file/cpd-3-19-2007.pdf |
id |
ftunivnantes:oai:HAL:hal-00330720v1 |
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record_format |
openpolar |
institution |
Open Polar |
collection |
Université de Nantes: HAL-UNIV-NANTES |
op_collection_id |
ftunivnantes |
language |
English |
topic |
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment [SDU.STU]Sciences of the Universe [physics]/Earth Sciences |
spellingShingle |
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment [SDU.STU]Sciences of the Universe [physics]/Earth Sciences Parrenin, F. Dreyfus, G. Durand, Geoffroy Fujita, S. Gagliardini, O. Gillet, F. Jouzel, Jean Kawamura, K. Lhomme, N. Masson-Delmotte, Valérie Ritz, C. Schwander, J. Shoji, H. Uemura, R. Watanabe, O. Yoshida, N. Ice flow modelling at EPICA Dome C and Dome Fuji, East Antarctica |
topic_facet |
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment [SDU.STU]Sciences of the Universe [physics]/Earth Sciences |
description |
International audience 1-D ice flow models are used to construct the age scales at the Dome C and Dome Fuji drilling sites (East Antarctica). The poorly constrained glaciological parameters at each site are recovered by fitting independent age markers identified on each core. We reconstruct past accumulation rates, that are larger than those modelled using the classical vapour saturation pressure relationship during glacial periods by up to a factor 1.5. During the Early Holocene, changes in reconstructed accumulation are not linearly related to changes in ice isotopic composition. A simple model of past elevation changes is developed and shows an amplitude variation of 110–120 m at both sites. We suggest that there is basal melting at Dome C (0.56±0.19 mm/yr). The reconstructed velocity profile is highly non linear at both sites, which suggests complex ice flow effects. This induces a non linear thinning function in both drilling sites, which is also characterized by bumps corresponding to variations in surface elevation with time. |
author2 |
Laboratoire de glaciologie et géophysique de l'environnement (LGGE) Observatoire des Sciences de l'Univers de Grenoble (OSUG) Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS) Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS) Niels Bohr Institute Copenhagen (NBI) Faculty of Science Copenhagen University of Copenhagen = Københavns Universitet (UCPH)-University of Copenhagen = Københavns Universitet (UCPH) National Institute of Polar Research Tokyo (NiPR) Center for Atmospheric and Oceanic Studies Sendai Tohoku University Sendai Physics Institute New Energy Resources Research Center Frontier Collaborative Research Center (FCRC) Tokyo Institute of Technology Tokyo (TITECH) |
format |
Article in Journal/Newspaper |
author |
Parrenin, F. Dreyfus, G. Durand, Geoffroy Fujita, S. Gagliardini, O. Gillet, F. Jouzel, Jean Kawamura, K. Lhomme, N. Masson-Delmotte, Valérie Ritz, C. Schwander, J. Shoji, H. Uemura, R. Watanabe, O. Yoshida, N. |
author_facet |
Parrenin, F. Dreyfus, G. Durand, Geoffroy Fujita, S. Gagliardini, O. Gillet, F. Jouzel, Jean Kawamura, K. Lhomme, N. Masson-Delmotte, Valérie Ritz, C. Schwander, J. Shoji, H. Uemura, R. Watanabe, O. Yoshida, N. |
author_sort |
Parrenin, F. |
title |
Ice flow modelling at EPICA Dome C and Dome Fuji, East Antarctica |
title_short |
Ice flow modelling at EPICA Dome C and Dome Fuji, East Antarctica |
title_full |
Ice flow modelling at EPICA Dome C and Dome Fuji, East Antarctica |
title_fullStr |
Ice flow modelling at EPICA Dome C and Dome Fuji, East Antarctica |
title_full_unstemmed |
Ice flow modelling at EPICA Dome C and Dome Fuji, East Antarctica |
title_sort |
ice flow modelling at epica dome c and dome fuji, east antarctica |
publisher |
HAL CCSD |
publishDate |
2007 |
url |
https://hal.science/hal-00330720 https://hal.science/hal-00330720/document https://hal.science/hal-00330720/file/cpd-3-19-2007.pdf |
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 EPICA |
genre_facet |
Antarc* Antarctica East Antarctica EPICA |
op_source |
ISSN: 1814-9340 EISSN: 1814-9359 Climate of the Past Discussions https://hal.science/hal-00330720 Climate of the Past Discussions, 2007, 3 (1), pp.19-61 |
op_relation |
hal-00330720 https://hal.science/hal-00330720 https://hal.science/hal-00330720/document https://hal.science/hal-00330720/file/cpd-3-19-2007.pdf |
op_rights |
info:eu-repo/semantics/OpenAccess |
_version_ |
1766065203078758400 |
spelling |
ftunivnantes:oai:HAL:hal-00330720v1 2023-05-15T13:35:24+02:00 Ice flow modelling at EPICA Dome C and Dome Fuji, East Antarctica Parrenin, F. Dreyfus, G. Durand, Geoffroy Fujita, S. Gagliardini, O. Gillet, F. Jouzel, Jean Kawamura, K. Lhomme, N. Masson-Delmotte, Valérie Ritz, C. Schwander, J. Shoji, H. Uemura, R. Watanabe, O. Yoshida, N. Laboratoire de glaciologie et géophysique de l'environnement (LGGE) Observatoire des Sciences de l'Univers de Grenoble (OSUG) Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS) Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS) Niels Bohr Institute Copenhagen (NBI) Faculty of Science Copenhagen University of Copenhagen = Københavns Universitet (UCPH)-University of Copenhagen = Københavns Universitet (UCPH) National Institute of Polar Research Tokyo (NiPR) Center for Atmospheric and Oceanic Studies Sendai Tohoku University Sendai Physics Institute New Energy Resources Research Center Frontier Collaborative Research Center (FCRC) Tokyo Institute of Technology Tokyo (TITECH) 2007-01-16 https://hal.science/hal-00330720 https://hal.science/hal-00330720/document https://hal.science/hal-00330720/file/cpd-3-19-2007.pdf en eng HAL CCSD European Geosciences Union (EGU) hal-00330720 https://hal.science/hal-00330720 https://hal.science/hal-00330720/document https://hal.science/hal-00330720/file/cpd-3-19-2007.pdf info:eu-repo/semantics/OpenAccess ISSN: 1814-9340 EISSN: 1814-9359 Climate of the Past Discussions https://hal.science/hal-00330720 Climate of the Past Discussions, 2007, 3 (1), pp.19-61 [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment [SDU.STU]Sciences of the Universe [physics]/Earth Sciences info:eu-repo/semantics/article Journal articles 2007 ftunivnantes 2023-02-08T04:17:01Z International audience 1-D ice flow models are used to construct the age scales at the Dome C and Dome Fuji drilling sites (East Antarctica). The poorly constrained glaciological parameters at each site are recovered by fitting independent age markers identified on each core. We reconstruct past accumulation rates, that are larger than those modelled using the classical vapour saturation pressure relationship during glacial periods by up to a factor 1.5. During the Early Holocene, changes in reconstructed accumulation are not linearly related to changes in ice isotopic composition. A simple model of past elevation changes is developed and shows an amplitude variation of 110–120 m at both sites. We suggest that there is basal melting at Dome C (0.56±0.19 mm/yr). The reconstructed velocity profile is highly non linear at both sites, which suggests complex ice flow effects. This induces a non linear thinning function in both drilling sites, which is also characterized by bumps corresponding to variations in surface elevation with time. Article in Journal/Newspaper Antarc* Antarctica East Antarctica EPICA Université de Nantes: HAL-UNIV-NANTES Dome Fuji ENVELOPE(39.700,39.700,-77.317,-77.317) East Antarctica |