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...

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Main Authors: 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.
Other Authors: 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)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)), Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA), 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: Report
Language:English
Published: HAL CCSD 2008
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
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spelling ftinsu:oai:HAL:hal-00330720v1 2024-04-28T08:02:14+00:00 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)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA) 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) 2008-06-18 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 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 https://hal.science/hal-00330720 2008 [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment [SDU.STU]Sciences of the Universe [physics]/Earth Sciences info:eu-repo/semantics/preprint Preprints, Working Papers, . 2008 ftinsu 2024-04-05T00:36:33Z 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. Report Antarc* Antarctica East Antarctica EPICA Institut national des sciences de l'Univers: HAL-INSU
institution Open Polar
collection Institut national des sciences de l'Univers: HAL-INSU
op_collection_id ftinsu
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)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA))
Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)
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 Report
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 2008
url https://hal.science/hal-00330720
https://hal.science/hal-00330720/document
https://hal.science/hal-00330720/file/cpd-3-19-2007.pdf
genre Antarc*
Antarctica
East Antarctica
EPICA
genre_facet Antarc*
Antarctica
East Antarctica
EPICA
op_source https://hal.science/hal-00330720
2008
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
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