Punctuated shutdown of Atlantic Meridional Overturning circulation during Greenland Stadial 1

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 runof that caused a sustained reduction of North Atlantic Meridional Overturning Circulation (AMOC), resulting in an antiphase temperature res...

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Published in:Scientific Reports
Main Authors: Hogg, Alan G., Southon, John R., Turney, Chris S.M., Palmer, Jonathan, Bronk Ramsey, Christopher, Fenwick, Pavla, Boswijk, Gretel, Friedrich, Michael, Helle, Gerhard, Hughen, Konrad, Jones, Richard, Kromer, Bernd, Noronha, Alexandra, Reynard, Linda, Staff, Richard, Wacker, Lukas
Format: Article in Journal/Newspaper
Language:English
Published: Nature Publishing Group/Macmillan Publishers Limited 2016
Subjects:
Online Access:https://hdl.handle.net/10289/10272
https://doi.org/10.1038/srep25902
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spelling ftunivwaikato:oai:researchcommons.waikato.ac.nz:10289/10272 2023-10-09T21:51:58+02:00 Punctuated shutdown of Atlantic Meridional Overturning circulation during Greenland Stadial 1 Hogg, Alan G. Southon, John R. Turney, Chris S.M. Palmer, Jonathan Bronk Ramsey, Christopher Fenwick, Pavla Boswijk, Gretel Friedrich, Michael Helle, Gerhard Hughen, Konrad Jones, Richard Kromer, Bernd Noronha, Alexandra Reynard, Linda Staff, Richard Wacker, Lukas 2016 application/pdf https://hdl.handle.net/10289/10272 https://doi.org/10.1038/srep25902 en eng Nature Publishing Group/Macmillan Publishers Limited Scientific Reports Hogg, A. G., Southon, J., Turney, C., Palmer, J., Bronk Ramsey, C., Fenwick, P., … Wacker, L. (2016). Punctuated shutdown of Atlantic Meridional Overturning circulation during Greenland Stadial 1. Scientific Reports, 6(25902). http://doi.org/10.1038/srep25902 2045-2322 https://hdl.handle.net/10289/10272 doi:10.1038/srep25902 This work is licensed under a Creative Commons Attribution 4.0 International License. Journal Article 2016 ftunivwaikato https://doi.org/10.1038/srep25902 2023-09-19T17:23:57Z 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 runof 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 frst 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 ofset 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 fndings suggest opposing hemispheric temperature trends were driven by atmospheric teleconnections, rather than AMOC changes. Article in Journal/Newspaper Greenland North Atlantic Southern Ocean The University of Waikato: Research Commons Greenland New Zealand Southern Ocean Scientific Reports 6 1
institution Open Polar
collection The University of Waikato: Research Commons
op_collection_id ftunivwaikato
language English
description 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 runof 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 frst 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 ofset 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 fndings suggest opposing hemispheric temperature trends were driven by atmospheric teleconnections, rather than AMOC changes.
format Article in Journal/Newspaper
author Hogg, Alan G.
Southon, John R.
Turney, Chris S.M.
Palmer, Jonathan
Bronk Ramsey, Christopher
Fenwick, Pavla
Boswijk, Gretel
Friedrich, Michael
Helle, Gerhard
Hughen, Konrad
Jones, Richard
Kromer, Bernd
Noronha, Alexandra
Reynard, Linda
Staff, Richard
Wacker, Lukas
spellingShingle Hogg, Alan G.
Southon, John R.
Turney, Chris S.M.
Palmer, Jonathan
Bronk Ramsey, Christopher
Fenwick, Pavla
Boswijk, Gretel
Friedrich, Michael
Helle, Gerhard
Hughen, Konrad
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, Chris S.M.
Palmer, Jonathan
Bronk Ramsey, Christopher
Fenwick, Pavla
Boswijk, Gretel
Friedrich, Michael
Helle, Gerhard
Hughen, Konrad
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/Macmillan Publishers Limited
publishDate 2016
url https://hdl.handle.net/10289/10272
https://doi.org/10.1038/srep25902
geographic Greenland
New Zealand
Southern Ocean
geographic_facet Greenland
New Zealand
Southern Ocean
genre Greenland
North Atlantic
Southern Ocean
genre_facet Greenland
North Atlantic
Southern Ocean
op_relation Scientific Reports
Hogg, A. G., Southon, J., Turney, C., Palmer, J., Bronk Ramsey, C., Fenwick, P., … Wacker, L. (2016). Punctuated shutdown of Atlantic Meridional Overturning circulation during Greenland Stadial 1. Scientific Reports, 6(25902). http://doi.org/10.1038/srep25902
2045-2322
https://hdl.handle.net/10289/10272
doi:10.1038/srep25902
op_rights This work is licensed under a Creative Commons Attribution 4.0 International License.
op_doi https://doi.org/10.1038/srep25902
container_title Scientific Reports
container_volume 6
container_issue 1
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