Implementation of counted layers for coherent ice core chronology
International audience A recent coherent chronology has been built for four Antarctic ice cores and the NorthGRIP (NGRIP) Greenland ice core (Antarctic Ice Core Chronology 2012, AICC2012) using a Bayesian approach for ice core dating (Datice). When building the AICC2012 chronology, and in order to p...
Published in: | Climate of the Past |
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Main Authors: | , , , , , , , |
Other Authors: | , , , , , , , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
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HAL CCSD
2015
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Online Access: | https://insu.hal.science/insu-01203665 https://insu.hal.science/insu-01203665/document https://insu.hal.science/insu-01203665/file/CLIMATE%20OF%20THE%20PAST%20-%20%20Implementation%20of%20counted%20layers%20for%20coherent%20ice%20core%20chronology.pdf https://doi.org/10.5194/cp-11-959-2015 |
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ftuniparissaclay:oai:HAL:insu-01203665v1 |
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openpolar |
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Open Polar |
collection |
Archives ouvertes de Paris-Saclay |
op_collection_id |
ftuniparissaclay |
language |
English |
topic |
[SDE]Environmental Sciences [MATH.MATH-NA]Mathematics [math]/Numerical Analysis [math.NA] |
spellingShingle |
[SDE]Environmental Sciences [MATH.MATH-NA]Mathematics [math]/Numerical Analysis [math.NA] Lemieux-Dudon, Bénédicte Bazin, Lucie Landais, Amaelle Kele, Habib Toye Mahamadou Guillevic, Myriam Kindler, Philippe Parrenin, Frédéric Martinerie, Patricia Implementation of counted layers for coherent ice core chronology |
topic_facet |
[SDE]Environmental Sciences [MATH.MATH-NA]Mathematics [math]/Numerical Analysis [math.NA] |
description |
International audience A recent coherent chronology has been built for four Antarctic ice cores and the NorthGRIP (NGRIP) Greenland ice core (Antarctic Ice Core Chronology 2012, AICC2012) using a Bayesian approach for ice core dating (Datice). When building the AICC2012 chronology, and in order to prevent any confusion with official ice core chronology, the AICC2012 chronology for NGRIP was forced to fit exactly the GICC05 chronology based on layer counting. However, such a strong tuning did not satisfy the hypothesis of independence of background parameters and observations for the NGRIP core, as required by Datice. We present here the implementation in Datice of a new type of markers that is better suited for constraints deduced from layer counting: the duration constraints. Estimating the global error on chronology due to such markers is not straightforward and implies some assumption on the correlation between individual counting errors for each interval of duration. We validate this new methodological implementation by conducting twin experiments and a posteriori diagnostics on the NGRIP ice core. Several sensitivity tests on marker sampling and correlation between counting errors were performed to provide some guidelines when using such a method for future dating experiments. Finally, using these markers for NGRIP in a five-core dating exercise with Datice leads to new chronologies that do not differ by more than 410 years from AICC2012 for Antarctic ice cores and 150 years from GICC05 for NGRIP over the last 60 000 years. |
author2 |
Mathematics and computing applied to oceanic and atmospheric flows (AIRSEA) Inria Grenoble - Rhône-Alpes Institut National de Recherche en Informatique et en Automatique (Inria)-Institut National de Recherche en Informatique et en Automatique (Inria)-Laboratoire Jean Kuntzmann (LJK) Université Pierre Mendès France - Grenoble 2 (UPMF)-Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Centre National de la Recherche Scientifique (CNRS)-Université Pierre Mendès France - Grenoble 2 (UPMF)-Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-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) Glaces et Continents, Climats et Isotopes Stables (GLACCIOS) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-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)) Niels Bohr Institute Copenhagen (NBI) Faculty of Science Copenhagen University of Copenhagen = Københavns Universitet (UCPH)-University of Copenhagen = Københavns Universitet (UCPH) Universität Bern = University of Bern = Université de Berne (UNIBE) 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) ANR-10-LABX-0018,L-IPSL,LabEx Institut Pierre Simon Laplace (IPSL): Understand climate and anticipate future changes(2010) |
format |
Article in Journal/Newspaper |
author |
Lemieux-Dudon, Bénédicte Bazin, Lucie Landais, Amaelle Kele, Habib Toye Mahamadou Guillevic, Myriam Kindler, Philippe Parrenin, Frédéric Martinerie, Patricia |
author_facet |
Lemieux-Dudon, Bénédicte Bazin, Lucie Landais, Amaelle Kele, Habib Toye Mahamadou Guillevic, Myriam Kindler, Philippe Parrenin, Frédéric Martinerie, Patricia |
author_sort |
Lemieux-Dudon, Bénédicte |
title |
Implementation of counted layers for coherent ice core chronology |
title_short |
Implementation of counted layers for coherent ice core chronology |
title_full |
Implementation of counted layers for coherent ice core chronology |
title_fullStr |
Implementation of counted layers for coherent ice core chronology |
title_full_unstemmed |
Implementation of counted layers for coherent ice core chronology |
title_sort |
implementation of counted layers for coherent ice core chronology |
publisher |
HAL CCSD |
publishDate |
2015 |
url |
https://insu.hal.science/insu-01203665 https://insu.hal.science/insu-01203665/document https://insu.hal.science/insu-01203665/file/CLIMATE%20OF%20THE%20PAST%20-%20%20Implementation%20of%20counted%20layers%20for%20coherent%20ice%20core%20chronology.pdf https://doi.org/10.5194/cp-11-959-2015 |
geographic |
Antarctic Greenland |
geographic_facet |
Antarctic Greenland |
genre |
Antarc* Antarctic Greenland Greenland ice core ice core NGRIP |
genre_facet |
Antarc* Antarctic Greenland Greenland ice core ice core NGRIP |
op_source |
ISSN: 1814-9324 EISSN: 1814-9332 Climate of the Past https://insu.hal.science/insu-01203665 Climate of the Past, 2015, 11 (6), pp.959-978. ⟨10.5194/cp-11-959-2015⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.5194/cp-11-959-2015 insu-01203665 https://insu.hal.science/insu-01203665 https://insu.hal.science/insu-01203665/document https://insu.hal.science/insu-01203665/file/CLIMATE%20OF%20THE%20PAST%20-%20%20Implementation%20of%20counted%20layers%20for%20coherent%20ice%20core%20chronology.pdf doi:10.5194/cp-11-959-2015 |
op_rights |
info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.5194/cp-11-959-2015 |
container_title |
Climate of the Past |
container_volume |
11 |
container_issue |
6 |
container_start_page |
959 |
op_container_end_page |
978 |
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1812177699500720128 |
spelling |
ftuniparissaclay:oai:HAL:insu-01203665v1 2024-10-06T13:42:53+00:00 Implementation of counted layers for coherent ice core chronology Lemieux-Dudon, Bénédicte Bazin, Lucie Landais, Amaelle Kele, Habib Toye Mahamadou Guillevic, Myriam Kindler, Philippe Parrenin, Frédéric Martinerie, Patricia Mathematics and computing applied to oceanic and atmospheric flows (AIRSEA) Inria Grenoble - Rhône-Alpes Institut National de Recherche en Informatique et en Automatique (Inria)-Institut National de Recherche en Informatique et en Automatique (Inria)-Laboratoire Jean Kuntzmann (LJK) Université Pierre Mendès France - Grenoble 2 (UPMF)-Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Centre National de la Recherche Scientifique (CNRS)-Université Pierre Mendès France - Grenoble 2 (UPMF)-Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-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) Glaces et Continents, Climats et Isotopes Stables (GLACCIOS) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-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)) Niels Bohr Institute Copenhagen (NBI) Faculty of Science Copenhagen University of Copenhagen = Københavns Universitet (UCPH)-University of Copenhagen = Københavns Universitet (UCPH) Universität Bern = University of Bern = Université de Berne (UNIBE) 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) ANR-10-LABX-0018,L-IPSL,LabEx Institut Pierre Simon Laplace (IPSL): Understand climate and anticipate future changes(2010) 2015-06 https://insu.hal.science/insu-01203665 https://insu.hal.science/insu-01203665/document https://insu.hal.science/insu-01203665/file/CLIMATE%20OF%20THE%20PAST%20-%20%20Implementation%20of%20counted%20layers%20for%20coherent%20ice%20core%20chronology.pdf https://doi.org/10.5194/cp-11-959-2015 en eng HAL CCSD European Geosciences Union (EGU) info:eu-repo/semantics/altIdentifier/doi/10.5194/cp-11-959-2015 insu-01203665 https://insu.hal.science/insu-01203665 https://insu.hal.science/insu-01203665/document https://insu.hal.science/insu-01203665/file/CLIMATE%20OF%20THE%20PAST%20-%20%20Implementation%20of%20counted%20layers%20for%20coherent%20ice%20core%20chronology.pdf doi:10.5194/cp-11-959-2015 info:eu-repo/semantics/OpenAccess ISSN: 1814-9324 EISSN: 1814-9332 Climate of the Past https://insu.hal.science/insu-01203665 Climate of the Past, 2015, 11 (6), pp.959-978. ⟨10.5194/cp-11-959-2015⟩ [SDE]Environmental Sciences [MATH.MATH-NA]Mathematics [math]/Numerical Analysis [math.NA] info:eu-repo/semantics/article Journal articles 2015 ftuniparissaclay https://doi.org/10.5194/cp-11-959-2015 2024-09-06T00:30:34Z International audience A recent coherent chronology has been built for four Antarctic ice cores and the NorthGRIP (NGRIP) Greenland ice core (Antarctic Ice Core Chronology 2012, AICC2012) using a Bayesian approach for ice core dating (Datice). When building the AICC2012 chronology, and in order to prevent any confusion with official ice core chronology, the AICC2012 chronology for NGRIP was forced to fit exactly the GICC05 chronology based on layer counting. However, such a strong tuning did not satisfy the hypothesis of independence of background parameters and observations for the NGRIP core, as required by Datice. We present here the implementation in Datice of a new type of markers that is better suited for constraints deduced from layer counting: the duration constraints. Estimating the global error on chronology due to such markers is not straightforward and implies some assumption on the correlation between individual counting errors for each interval of duration. We validate this new methodological implementation by conducting twin experiments and a posteriori diagnostics on the NGRIP ice core. Several sensitivity tests on marker sampling and correlation between counting errors were performed to provide some guidelines when using such a method for future dating experiments. Finally, using these markers for NGRIP in a five-core dating exercise with Datice leads to new chronologies that do not differ by more than 410 years from AICC2012 for Antarctic ice cores and 150 years from GICC05 for NGRIP over the last 60 000 years. Article in Journal/Newspaper Antarc* Antarctic Greenland Greenland ice core ice core NGRIP Archives ouvertes de Paris-Saclay Antarctic Greenland Climate of the Past 11 6 959 978 |