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...
Published in: | Scientific Reports |
---|---|
Main Authors: | , , , , , , , , , , , , , , , |
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 |
id |
ftunivwaikato:oai:researchcommons.waikato.ac.nz:10289/10272 |
---|---|
record_format |
openpolar |
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 |
_version_ |
1779315091761528832 |