Direct north-south synchronization of abrupt climate change record in ice cores using Beryllium 10

Gas is trapped in polar ice sheets at 50–120m below the surface and is therefore younger than the surrounding ice. Firn densification models are used to evaluate this ice age-gas age difference (1age) in the past. However, such models need to be validated by data, in particular for periods colder th...

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Main Authors: Raisbeck, G., Yiou, F., Jouzel, Jean, Stocker, T.F.
Other Authors: Centre de Spectrométrie Nucléaire et de Spectrométrie de Masse (CSNSM), Université Paris-Sud - Paris 11 (UP11)-Institut National de Physique Nucléaire et de Physique des Particules du CNRS (IN2P3)-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)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2007
Subjects:
geo
Online Access:http://hal.in2p3.fr/in2p3-00182754/file/cp-3-541-2007.pdf
http://hal.in2p3.fr/in2p3-00182754
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spelling fttriple:oai:gotriple.eu:10670/1.aomjxd 2023-05-15T14:03:11+02:00 Direct north-south synchronization of abrupt climate change record in ice cores using Beryllium 10 Raisbeck, G. Yiou, F. Jouzel, Jean Stocker, T.F. Centre de Spectrométrie Nucléaire et de Spectrométrie de Masse (CSNSM) Université Paris-Sud - Paris 11 (UP11)-Institut National de Physique Nucléaire et de Physique des Particules du CNRS (IN2P3)-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) 2007-01-01 http://hal.in2p3.fr/in2p3-00182754/file/cp-3-541-2007.pdf http://hal.in2p3.fr/in2p3-00182754 en eng HAL CCSD European Geosciences Union (EGU) in2p3-00182754 10670/1.aomjxd http://hal.in2p3.fr/in2p3-00182754/file/cp-3-541-2007.pdf http://hal.in2p3.fr/in2p3-00182754 Hyper Article en Ligne - Sciences de l'Homme et de la Société ISSN: 1814-9324 EISSN: 1814-9332 Climate of the Past Climate of the Past, European Geosciences Union (EGU), 2007, 3, pp.541-547 geo envir Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2007 fttriple 2023-01-22T17:26:54Z Gas is trapped in polar ice sheets at 50–120m below the surface and is therefore younger than the surrounding ice. Firn densification models are used to evaluate this ice age-gas age difference (1age) in the past. However, such models need to be validated by data, in particular for periods colder than present day on the East Antarctic plateau. Here we bring new constraints to test a firn densification model applied to the EPICA Dome C (EDC) site for the last 50 kyr, by linking the EDC ice core to the EPICA Dronning Maud Land (EDML) ice core, both in the ice phase (using volcanic horizons) and in the gas phase (using rapid methane variations). We also use the structured 10Be peak, occurring 41 kyr before present (BP) and due to the low geomagnetic field associated with the Laschamp event, to experimentally estimate the 1age during this event. Our results seem to reveal an overestimate of the 1age by the firn densification model during the last glacial period at EDC. Tests with different accumulation rates and temperature scenarios do not entirely resolve this discrepancy. Although the exact reasons for the 1age overestimate at the two EPICA sites remain unknown at this stage, we conclude that current densification model simulations have deficits under glacial climatic conditions. Whatever the cause of the 1age overestimate, our finding suggests that the phase relationship between CO2 and EDC temperature previously inferred for the start of the last deglaciation (lag of CO2 by 800±600 yr) seems to be overestimated. Article in Journal/Newspaper Antarc* Antarctic Dronning Maud Land EPICA ice core Unknown Antarctic Dronning Maud Land
institution Open Polar
collection Unknown
op_collection_id fttriple
language English
topic geo
envir
spellingShingle geo
envir
Raisbeck, G.
Yiou, F.
Jouzel, Jean
Stocker, T.F.
Direct north-south synchronization of abrupt climate change record in ice cores using Beryllium 10
topic_facet geo
envir
description Gas is trapped in polar ice sheets at 50–120m below the surface and is therefore younger than the surrounding ice. Firn densification models are used to evaluate this ice age-gas age difference (1age) in the past. However, such models need to be validated by data, in particular for periods colder than present day on the East Antarctic plateau. Here we bring new constraints to test a firn densification model applied to the EPICA Dome C (EDC) site for the last 50 kyr, by linking the EDC ice core to the EPICA Dronning Maud Land (EDML) ice core, both in the ice phase (using volcanic horizons) and in the gas phase (using rapid methane variations). We also use the structured 10Be peak, occurring 41 kyr before present (BP) and due to the low geomagnetic field associated with the Laschamp event, to experimentally estimate the 1age during this event. Our results seem to reveal an overestimate of the 1age by the firn densification model during the last glacial period at EDC. Tests with different accumulation rates and temperature scenarios do not entirely resolve this discrepancy. Although the exact reasons for the 1age overestimate at the two EPICA sites remain unknown at this stage, we conclude that current densification model simulations have deficits under glacial climatic conditions. Whatever the cause of the 1age overestimate, our finding suggests that the phase relationship between CO2 and EDC temperature previously inferred for the start of the last deglaciation (lag of CO2 by 800±600 yr) seems to be overestimated.
author2 Centre de Spectrométrie Nucléaire et de Spectrométrie de Masse (CSNSM)
Université Paris-Sud - Paris 11 (UP11)-Institut National de Physique Nucléaire et de Physique des Particules du CNRS (IN2P3)-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)
format Article in Journal/Newspaper
author Raisbeck, G.
Yiou, F.
Jouzel, Jean
Stocker, T.F.
author_facet Raisbeck, G.
Yiou, F.
Jouzel, Jean
Stocker, T.F.
author_sort Raisbeck, G.
title Direct north-south synchronization of abrupt climate change record in ice cores using Beryllium 10
title_short Direct north-south synchronization of abrupt climate change record in ice cores using Beryllium 10
title_full Direct north-south synchronization of abrupt climate change record in ice cores using Beryllium 10
title_fullStr Direct north-south synchronization of abrupt climate change record in ice cores using Beryllium 10
title_full_unstemmed Direct north-south synchronization of abrupt climate change record in ice cores using Beryllium 10
title_sort direct north-south synchronization of abrupt climate change record in ice cores using beryllium 10
publisher HAL CCSD
publishDate 2007
url http://hal.in2p3.fr/in2p3-00182754/file/cp-3-541-2007.pdf
http://hal.in2p3.fr/in2p3-00182754
geographic Antarctic
Dronning Maud Land
geographic_facet Antarctic
Dronning Maud Land
genre Antarc*
Antarctic
Dronning Maud Land
EPICA
ice core
genre_facet Antarc*
Antarctic
Dronning Maud Land
EPICA
ice core
op_source Hyper Article en Ligne - Sciences de l'Homme et de la Société
ISSN: 1814-9324
EISSN: 1814-9332
Climate of the Past
Climate of the Past, European Geosciences Union (EGU), 2007, 3, pp.541-547
op_relation in2p3-00182754
10670/1.aomjxd
http://hal.in2p3.fr/in2p3-00182754/file/cp-3-541-2007.pdf
http://hal.in2p3.fr/in2p3-00182754
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