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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Published in:Climate of the Past
Main Authors: Loulergue, L., Parrenin, F., Blunier, T., Barnola, J.-M., Spahni, R., Schilt, A., Raisbeck, G., Chappellaz, J.
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/cp-3-527-2007
https://cp.copernicus.org/articles/3/527/2007/
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spelling ftcopernicus:oai:publications.copernicus.org:cp6261 2023-05-15T13:36:36+02:00 New constraints on the gas age-ice age difference along the EPICA ice cores, 0–50 kyr Loulergue, L. Parrenin, F. Blunier, T. Barnola, J.-M. Spahni, R. Schilt, A. Raisbeck, G. Chappellaz, J. 2018-09-27 application/pdf https://doi.org/10.5194/cp-3-527-2007 https://cp.copernicus.org/articles/3/527/2007/ eng eng doi:10.5194/cp-3-527-2007 https://cp.copernicus.org/articles/3/527/2007/ eISSN: 1814-9332 Text 2018 ftcopernicus https://doi.org/10.5194/cp-3-527-2007 2020-07-20T16:27:02Z 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. Text Antarc* Antarctic Dronning Maud Land EPICA ice core Copernicus Publications: E-Journals Antarctic Dronning Maud Land Climate of the Past 3 3 527 540
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
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 Text
author Loulergue, L.
Parrenin, F.
Blunier, T.
Barnola, J.-M.
Spahni, R.
Schilt, A.
Raisbeck, G.
Chappellaz, J.
spellingShingle Loulergue, L.
Parrenin, F.
Blunier, T.
Barnola, J.-M.
Spahni, R.
Schilt, A.
Raisbeck, G.
Chappellaz, J.
New constraints on the gas age-ice age difference along the EPICA ice cores, 0–50 kyr
author_facet Loulergue, L.
Parrenin, F.
Blunier, T.
Barnola, J.-M.
Spahni, R.
Schilt, A.
Raisbeck, G.
Chappellaz, J.
author_sort Loulergue, L.
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
publishDate 2018
url https://doi.org/10.5194/cp-3-527-2007
https://cp.copernicus.org/articles/3/527/2007/
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 eISSN: 1814-9332
op_relation doi:10.5194/cp-3-527-2007
https://cp.copernicus.org/articles/3/527/2007/
op_doi https://doi.org/10.5194/cp-3-527-2007
container_title Climate of the Past
container_volume 3
container_issue 3
container_start_page 527
op_container_end_page 540
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