Punctuated shutdown of Atlantic Meridional Overturning Circulation during Greenland Stadial 1
© The Author(s), 2016. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Scientific Reports 6 (2016): 25902, doi:10.1038/srep25902. The Greenland Stadial 1 (GS-1; ~12.9 to 11.65 kyr cal BP) was a period of North Atlantic...
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ftwhoas:oai:darchive.mblwhoilibrary.org:1912/8047 2023-05-15T16:28:41+02:00 Punctuated shutdown of Atlantic Meridional Overturning Circulation during Greenland Stadial 1 Hogg, Alan G. Southon, John R. Turney, Christian S. M. Palmer, Jonathan G. Bronk Ramsey, Christopher Fenwick, Pavla Boswijk, Gretel Friedrich, Michael Helle, Gerhard Hughen, Konrad A. Jones, Richard Kromer, Bernd Noronha, Alexandra Reynard, Linda Staff, Richard Wacker, Lukas 2016-05-19 https://hdl.handle.net/1912/8047 en_US eng Nature Publishing Group https://doi.org/10.1038/srep25902 Scientific Reports 6 (2016): 25902 https://hdl.handle.net/1912/8047 doi:10.1038/srep25902 Attribution 4.0 International http://creativecommons.org/licenses/by/4.0/ CC-BY Scientific Reports 6 (2016): 25902 doi:10.1038/srep25902 Article 2016 ftwhoas https://doi.org/10.1038/srep25902 2022-05-28T22:59:34Z © The Author(s), 2016. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Scientific Reports 6 (2016): 25902, doi:10.1038/srep25902. The Greenland Stadial 1 (GS-1; ~12.9 to 11.65 kyr cal BP) was a period of North Atlantic cooling, thought to have been initiated by North America fresh water runoff that caused a sustained reduction of North Atlantic Meridional Overturning Circulation (AMOC), resulting in an antiphase temperature response between the hemispheres (the ‘bipolar seesaw’). Here we exploit sub-fossil New Zealand kauri trees to report the first securely dated, decadally-resolved atmospheric radiocarbon (14C) record spanning GS-1. By precisely aligning Southern and Northern Hemisphere tree-ring 14C records with marine 14C sequences we document two relatively short periods of AMOC collapse during the stadial, at ~12,920-12,640 cal BP and 12,050-11,900 cal BP. In addition, our data show that the interhemispheric atmospheric 14C offset was close to zero prior to GS-1, before reaching ‘near-modern’ values at ~12,660 cal BP, consistent with synchronous recovery of overturning in both hemispheres and increased Southern Ocean ventilation. Hence, sustained North Atlantic cooling across GS-1 was not driven by a prolonged AMOC reduction but probably due to an equatorward migration of the Polar Front, reducing the advection of southwesterly air masses to high latitudes. Our findings suggest opposing hemispheric temperature trends were driven by atmospheric teleconnections, rather than AMOC changes. This work was part funded by the Foundation for Research, Science and Technology (FRST)—now Ministry for Business, Innovation & Employment (MBIE)-PROP-20224-SFK-UOA), a Royal Society of New Zealand grant, the Australian Research Council (FL100100195 and DP0664898) and the Natural Environment Research Council (NE/H009922/1, NE/I007660/1, NER/A/S/2001/01037 and NE/H007865/1). Article in Journal/Newspaper Greenland North Atlantic Southern Ocean Woods Hole Scientific Community: WHOAS (Woods Hole Open Access Server) Southern Ocean Greenland New Zealand Ner ENVELOPE(6.622,6.622,62.612,62.612) Scientific Reports 6 1 |
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Woods Hole Scientific Community: WHOAS (Woods Hole Open Access Server) |
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© The Author(s), 2016. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Scientific Reports 6 (2016): 25902, doi:10.1038/srep25902. The Greenland Stadial 1 (GS-1; ~12.9 to 11.65 kyr cal BP) was a period of North Atlantic cooling, thought to have been initiated by North America fresh water runoff that caused a sustained reduction of North Atlantic Meridional Overturning Circulation (AMOC), resulting in an antiphase temperature response between the hemispheres (the ‘bipolar seesaw’). Here we exploit sub-fossil New Zealand kauri trees to report the first securely dated, decadally-resolved atmospheric radiocarbon (14C) record spanning GS-1. By precisely aligning Southern and Northern Hemisphere tree-ring 14C records with marine 14C sequences we document two relatively short periods of AMOC collapse during the stadial, at ~12,920-12,640 cal BP and 12,050-11,900 cal BP. In addition, our data show that the interhemispheric atmospheric 14C offset was close to zero prior to GS-1, before reaching ‘near-modern’ values at ~12,660 cal BP, consistent with synchronous recovery of overturning in both hemispheres and increased Southern Ocean ventilation. Hence, sustained North Atlantic cooling across GS-1 was not driven by a prolonged AMOC reduction but probably due to an equatorward migration of the Polar Front, reducing the advection of southwesterly air masses to high latitudes. Our findings suggest opposing hemispheric temperature trends were driven by atmospheric teleconnections, rather than AMOC changes. This work was part funded by the Foundation for Research, Science and Technology (FRST)—now Ministry for Business, Innovation & Employment (MBIE)-PROP-20224-SFK-UOA), a Royal Society of New Zealand grant, the Australian Research Council (FL100100195 and DP0664898) and the Natural Environment Research Council (NE/H009922/1, NE/I007660/1, NER/A/S/2001/01037 and NE/H007865/1). |
format |
Article in Journal/Newspaper |
author |
Hogg, Alan G. Southon, John R. Turney, Christian S. M. Palmer, Jonathan G. Bronk Ramsey, Christopher Fenwick, Pavla Boswijk, Gretel Friedrich, Michael Helle, Gerhard Hughen, Konrad A. Jones, Richard Kromer, Bernd Noronha, Alexandra Reynard, Linda Staff, Richard Wacker, Lukas |
spellingShingle |
Hogg, Alan G. Southon, John R. Turney, Christian S. M. Palmer, Jonathan G. Bronk Ramsey, Christopher Fenwick, Pavla Boswijk, Gretel Friedrich, Michael Helle, Gerhard Hughen, Konrad A. Jones, Richard Kromer, Bernd Noronha, Alexandra Reynard, Linda Staff, Richard Wacker, Lukas Punctuated shutdown of Atlantic Meridional Overturning Circulation during Greenland Stadial 1 |
author_facet |
Hogg, Alan G. Southon, John R. Turney, Christian S. M. Palmer, Jonathan G. Bronk Ramsey, Christopher Fenwick, Pavla Boswijk, Gretel Friedrich, Michael Helle, Gerhard Hughen, Konrad A. Jones, Richard Kromer, Bernd Noronha, Alexandra Reynard, Linda Staff, Richard Wacker, Lukas |
author_sort |
Hogg, Alan G. |
title |
Punctuated shutdown of Atlantic Meridional Overturning Circulation during Greenland Stadial 1 |
title_short |
Punctuated shutdown of Atlantic Meridional Overturning Circulation during Greenland Stadial 1 |
title_full |
Punctuated shutdown of Atlantic Meridional Overturning Circulation during Greenland Stadial 1 |
title_fullStr |
Punctuated shutdown of Atlantic Meridional Overturning Circulation during Greenland Stadial 1 |
title_full_unstemmed |
Punctuated shutdown of Atlantic Meridional Overturning Circulation during Greenland Stadial 1 |
title_sort |
punctuated shutdown of atlantic meridional overturning circulation during greenland stadial 1 |
publisher |
Nature Publishing Group |
publishDate |
2016 |
url |
https://hdl.handle.net/1912/8047 |
long_lat |
ENVELOPE(6.622,6.622,62.612,62.612) |
geographic |
Southern Ocean Greenland New Zealand Ner |
geographic_facet |
Southern Ocean Greenland New Zealand Ner |
genre |
Greenland North Atlantic Southern Ocean |
genre_facet |
Greenland North Atlantic Southern Ocean |
op_source |
Scientific Reports 6 (2016): 25902 doi:10.1038/srep25902 |
op_relation |
https://doi.org/10.1038/srep25902 Scientific Reports 6 (2016): 25902 https://hdl.handle.net/1912/8047 doi:10.1038/srep25902 |
op_rights |
Attribution 4.0 International http://creativecommons.org/licenses/by/4.0/ |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1038/srep25902 |
container_title |
Scientific Reports |
container_volume |
6 |
container_issue |
1 |
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1766018369143701504 |