New constraints on the gas age-ice age difference along the EPICA ice cores, 0–50 kyr
Gas is trapped in polar ice sheets at ~50–120 m below the surface and is therefore younger than the surrounding ice. Firn densification models are used to evaluate this ice age-gas age difference (Δage) in the past. However, such models need to be validated by data, in particular for periods colder...
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ftdoajarticles:oai:doaj.org/article:e020adb3620c443fa0401ceedfb17c30 2023-05-15T13:45:23+02:00 New constraints on the gas age-ice age difference along the EPICA ice cores, 0–50 kyr J. Chappellaz A. Schilt G. Raisbeck R. Spahni J.-M. Barnola T. Blunier F. Parrenin L. Loulergue 2007-08-01T00:00:00Z https://doaj.org/article/e020adb3620c443fa0401ceedfb17c30 EN eng Copernicus Publications http://www.clim-past.net/3/527/2007/cp-3-527-2007.pdf https://doaj.org/toc/1814-9324 https://doaj.org/toc/1814-9332 1814-9324 1814-9332 https://doaj.org/article/e020adb3620c443fa0401ceedfb17c30 Climate of the Past, Vol 3, Iss 3, Pp 527-540 (2007) Environmental pollution TD172-193.5 Environmental protection TD169-171.8 Environmental sciences GE1-350 article 2007 ftdoajarticles 2022-12-31T11:52:10Z Gas is trapped in polar ice sheets at ~50–120 m below the surface and is therefore younger than the surrounding ice. Firn densification models are used to evaluate this ice age-gas age difference (Δage) 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 10 Be peak, occurring 41 kyr before present (BP) and due to the low geomagnetic field associated with the Laschamp event, to experimentally estimate the Δage during this event. Our results seem to reveal an overestimate of the Δage 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 Δage 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 Δage overestimate, our finding suggests that the phase relationship between CO 2 and EDC temperature previously inferred for the start of the last deglaciation (lag of CO 2 by 800±600 yr) seems to be overestimated. Article in Journal/Newspaper Antarc* Antarctic Dronning Maud Land EPICA ice core Directory of Open Access Journals: DOAJ Articles Antarctic Dronning Maud Land |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Environmental pollution TD172-193.5 Environmental protection TD169-171.8 Environmental sciences GE1-350 |
spellingShingle |
Environmental pollution TD172-193.5 Environmental protection TD169-171.8 Environmental sciences GE1-350 J. Chappellaz A. Schilt G. Raisbeck R. Spahni J.-M. Barnola T. Blunier F. Parrenin L. Loulergue New constraints on the gas age-ice age difference along the EPICA ice cores, 0–50 kyr |
topic_facet |
Environmental pollution TD172-193.5 Environmental protection TD169-171.8 Environmental sciences GE1-350 |
description |
Gas is trapped in polar ice sheets at ~50–120 m below the surface and is therefore younger than the surrounding ice. Firn densification models are used to evaluate this ice age-gas age difference (Δage) 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 10 Be peak, occurring 41 kyr before present (BP) and due to the low geomagnetic field associated with the Laschamp event, to experimentally estimate the Δage during this event. Our results seem to reveal an overestimate of the Δage 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 Δage 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 Δage overestimate, our finding suggests that the phase relationship between CO 2 and EDC temperature previously inferred for the start of the last deglaciation (lag of CO 2 by 800±600 yr) seems to be overestimated. |
format |
Article in Journal/Newspaper |
author |
J. Chappellaz A. Schilt G. Raisbeck R. Spahni J.-M. Barnola T. Blunier F. Parrenin L. Loulergue |
author_facet |
J. Chappellaz A. Schilt G. Raisbeck R. Spahni J.-M. Barnola T. Blunier F. Parrenin L. Loulergue |
author_sort |
J. Chappellaz |
title |
New constraints on the gas age-ice age difference along the EPICA ice cores, 0–50 kyr |
title_short |
New constraints on the gas age-ice age difference along the EPICA ice cores, 0–50 kyr |
title_full |
New constraints on the gas age-ice age difference along the EPICA ice cores, 0–50 kyr |
title_fullStr |
New constraints on the gas age-ice age difference along the EPICA ice cores, 0–50 kyr |
title_full_unstemmed |
New constraints on the gas age-ice age difference along the EPICA ice cores, 0–50 kyr |
title_sort |
new constraints on the gas age-ice age difference along the epica ice cores, 0–50 kyr |
publisher |
Copernicus Publications |
publishDate |
2007 |
url |
https://doaj.org/article/e020adb3620c443fa0401ceedfb17c30 |
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 |
Climate of the Past, Vol 3, Iss 3, Pp 527-540 (2007) |
op_relation |
http://www.clim-past.net/3/527/2007/cp-3-527-2007.pdf https://doaj.org/toc/1814-9324 https://doaj.org/toc/1814-9332 1814-9324 1814-9332 https://doaj.org/article/e020adb3620c443fa0401ceedfb17c30 |
_version_ |
1766223463327989760 |