Abrupt rise in atmospheric CO 2 at the onset of the Bølling/Allerød: in-situ ice core data versus true atmospheric signals

During the last glacial/interglacial transition the Earth's climate underwent abrupt changes around 14.6 kyr ago. Temperature proxies from ice cores revealed the onset of the Bølling/Allerød (B/A) warm period in the north and the start of the Antarctic Cold Reversal in the south. Furthermore, t...

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Published in:Climate of the Past
Main Authors: J. Chappellaz, A. Lourantou, D. Buiron, P. Köhler, G. Knorr
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2011
Subjects:
Online Access:https://doi.org/10.5194/cp-7-473-2011
https://doaj.org/article/7117fc70371a45d0aadb8b803bf7959a
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spelling ftdoajarticles:oai:doaj.org/article:7117fc70371a45d0aadb8b803bf7959a 2023-05-15T14:00:08+02:00 Abrupt rise in atmospheric CO 2 at the onset of the Bølling/Allerød: in-situ ice core data versus true atmospheric signals J. Chappellaz A. Lourantou D. Buiron P. Köhler G. Knorr 2011-05-01T00:00:00Z https://doi.org/10.5194/cp-7-473-2011 https://doaj.org/article/7117fc70371a45d0aadb8b803bf7959a EN eng Copernicus Publications http://www.clim-past.net/7/473/2011/cp-7-473-2011.pdf https://doaj.org/toc/1814-9324 https://doaj.org/toc/1814-9332 doi:10.5194/cp-7-473-2011 1814-9324 1814-9332 https://doaj.org/article/7117fc70371a45d0aadb8b803bf7959a Climate of the Past, Vol 7, Iss 2, Pp 473-486 (2011) Environmental pollution TD172-193.5 Environmental protection TD169-171.8 Environmental sciences GE1-350 article 2011 ftdoajarticles https://doi.org/10.5194/cp-7-473-2011 2022-12-31T13:44:33Z During the last glacial/interglacial transition the Earth's climate underwent abrupt changes around 14.6 kyr ago. Temperature proxies from ice cores revealed the onset of the Bølling/Allerød (B/A) warm period in the north and the start of the Antarctic Cold Reversal in the south. Furthermore, the B/A was accompanied by a rapid sea level rise of about 20 m during meltwater pulse (MWP) 1A, whose exact timing is a matter of current debate. In-situ measured CO 2 in the EPICA Dome C (EDC) ice core also revealed a remarkable jump of 10 ± 1 ppmv in 230 yr at the same time. Allowing for the modelled age distribution of CO 2 in firn, we show that atmospheric CO 2 could have jumped by 20–35 ppmv in less than 200 yr, which is a factor of 2–3.5 greater than the CO 2 signal recorded in-situ in EDC. This rate of change in atmospheric CO 2 corresponds to 29–50% of the anthropogenic signal during the last 50 yr and is connected with a radiative forcing of 0.59–0.75 W m −2 . Using a model-based airborne fraction of 0.17 of atmospheric CO 2 , we infer that 125 Pg of carbon need to be released into the atmosphere to produce such a peak. If the abrupt rise in CO 2 at the onset of the B/A is unique with respect to other Dansgaard/Oeschger (D/O) events of the last 60 kyr (which seems plausible if not unequivocal based on current observations), then the mechanism responsible for it may also have been unique. Available δ 13 CO 2 data are neutral, whether the source of the carbon is of marine or terrestrial origin. We therefore hypothesise that most of the carbon might have been activated as a consequence of continental shelf flooding during MWP-1A. This potential impact of rapid sea level rise on atmospheric CO 2 might define the point of no return during the last deglaciation. Article in Journal/Newspaper Antarc* Antarctic EPICA ice core Directory of Open Access Journals: DOAJ Articles Antarctic The Antarctic Climate of the Past 7 2 473 486
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. Lourantou
D. Buiron
P. Köhler
G. Knorr
Abrupt rise in atmospheric CO 2 at the onset of the Bølling/Allerød: in-situ ice core data versus true atmospheric signals
topic_facet Environmental pollution
TD172-193.5
Environmental protection
TD169-171.8
Environmental sciences
GE1-350
description During the last glacial/interglacial transition the Earth's climate underwent abrupt changes around 14.6 kyr ago. Temperature proxies from ice cores revealed the onset of the Bølling/Allerød (B/A) warm period in the north and the start of the Antarctic Cold Reversal in the south. Furthermore, the B/A was accompanied by a rapid sea level rise of about 20 m during meltwater pulse (MWP) 1A, whose exact timing is a matter of current debate. In-situ measured CO 2 in the EPICA Dome C (EDC) ice core also revealed a remarkable jump of 10 ± 1 ppmv in 230 yr at the same time. Allowing for the modelled age distribution of CO 2 in firn, we show that atmospheric CO 2 could have jumped by 20–35 ppmv in less than 200 yr, which is a factor of 2–3.5 greater than the CO 2 signal recorded in-situ in EDC. This rate of change in atmospheric CO 2 corresponds to 29–50% of the anthropogenic signal during the last 50 yr and is connected with a radiative forcing of 0.59–0.75 W m −2 . Using a model-based airborne fraction of 0.17 of atmospheric CO 2 , we infer that 125 Pg of carbon need to be released into the atmosphere to produce such a peak. If the abrupt rise in CO 2 at the onset of the B/A is unique with respect to other Dansgaard/Oeschger (D/O) events of the last 60 kyr (which seems plausible if not unequivocal based on current observations), then the mechanism responsible for it may also have been unique. Available δ 13 CO 2 data are neutral, whether the source of the carbon is of marine or terrestrial origin. We therefore hypothesise that most of the carbon might have been activated as a consequence of continental shelf flooding during MWP-1A. This potential impact of rapid sea level rise on atmospheric CO 2 might define the point of no return during the last deglaciation.
format Article in Journal/Newspaper
author J. Chappellaz
A. Lourantou
D. Buiron
P. Köhler
G. Knorr
author_facet J. Chappellaz
A. Lourantou
D. Buiron
P. Köhler
G. Knorr
author_sort J. Chappellaz
title Abrupt rise in atmospheric CO 2 at the onset of the Bølling/Allerød: in-situ ice core data versus true atmospheric signals
title_short Abrupt rise in atmospheric CO 2 at the onset of the Bølling/Allerød: in-situ ice core data versus true atmospheric signals
title_full Abrupt rise in atmospheric CO 2 at the onset of the Bølling/Allerød: in-situ ice core data versus true atmospheric signals
title_fullStr Abrupt rise in atmospheric CO 2 at the onset of the Bølling/Allerød: in-situ ice core data versus true atmospheric signals
title_full_unstemmed Abrupt rise in atmospheric CO 2 at the onset of the Bølling/Allerød: in-situ ice core data versus true atmospheric signals
title_sort abrupt rise in atmospheric co 2 at the onset of the bølling/allerød: in-situ ice core data versus true atmospheric signals
publisher Copernicus Publications
publishDate 2011
url https://doi.org/10.5194/cp-7-473-2011
https://doaj.org/article/7117fc70371a45d0aadb8b803bf7959a
geographic Antarctic
The Antarctic
geographic_facet Antarctic
The Antarctic
genre Antarc*
Antarctic
EPICA
ice core
genre_facet Antarc*
Antarctic
EPICA
ice core
op_source Climate of the Past, Vol 7, Iss 2, Pp 473-486 (2011)
op_relation http://www.clim-past.net/7/473/2011/cp-7-473-2011.pdf
https://doaj.org/toc/1814-9324
https://doaj.org/toc/1814-9332
doi:10.5194/cp-7-473-2011
1814-9324
1814-9332
https://doaj.org/article/7117fc70371a45d0aadb8b803bf7959a
op_doi https://doi.org/10.5194/cp-7-473-2011
container_title Climate of the Past
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container_issue 2
container_start_page 473
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