Relative timing of precipitation and ocean circulation changes in the western equatorial Atlantic over the last 45 kyr
International audience Thanks to its optimal location on the northern Brazilian margin, core MD09-3257 records both ocean circulation and atmospheric changes. The latter occur locally in the form of increased rainfall on the adjacent continent during the cold intervals recorded in Greenland ice and...
Published in: | Climate of the Past |
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Main Authors: | , , , , , , , , , , , , , |
Other Authors: | , , , , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
HAL CCSD
2018
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Subjects: | |
Online Access: | https://hal.archives-ouvertes.fr/hal-02407248 https://hal.archives-ouvertes.fr/hal-02407248/document https://hal.archives-ouvertes.fr/hal-02407248/file/cp-14-1315-2018.pdf https://doi.org/10.5194/cp-14-1315-2018 |
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ftunivnantes:oai:HAL:hal-02407248v1 |
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openpolar |
institution |
Open Polar |
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Université de Nantes: HAL-UNIV-NANTES |
op_collection_id |
ftunivnantes |
language |
English |
topic |
Panoply [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology |
spellingShingle |
Panoply [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology Waelbroeck, Claire Pichat, Sylvain Böhm, Evelyn Lougheed, Bryan C. Faranda, Davide Vrac, Mathieu Missiaen, Lise Vázquez Riveiros, Natalia Burckel, Pierre Lippold, Jörg Arz, Helge W. Dokken, Trond Thil, François Dapoigny, Arnaud Relative timing of precipitation and ocean circulation changes in the western equatorial Atlantic over the last 45 kyr |
topic_facet |
Panoply [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology |
description |
International audience Thanks to its optimal location on the northern Brazilian margin, core MD09-3257 records both ocean circulation and atmospheric changes. The latter occur locally in the form of increased rainfall on the adjacent continent during the cold intervals recorded in Greenland ice and northern North Atlantic sediment cores (i.e., Greenland stadi-als). These rainfall events are recorded in MD09-3257 as peaks in ln(Ti / Ca). New sedimentary Pa / Th data indicate that mid-depth western equatorial water mass transport decreased during all of the Greenland stadials of the last 40 kyr. Using cross-wavelet transforms and spectrogram analysis, we assess the relative phase between the MD09-3257 sed-imentary Pa / Th and ln(Ti / Ca) signals. We show that decreased water mass transport between a depth of ∼ 1300 and 2300 m in the western equatorial Atlantic preceded increased rainfall over the adjacent continent by 120 to 400 yr at Dansgaard-Oeschger (D-O) frequencies, and by 280 to 980 yr at Heinrich-like frequencies. We suggest that the large lead of ocean circulation changes with respect to changes in tropical South American precipitation at Heinrich-like frequencies is related to the effect of a positive feedback involving iceberg discharges in the North Atlantic. In contrast, the absence of widespread ice rafted detrital layers in North Atlantic cores during DO stadials supports the hypothesis that a feedback such as this was not triggered in the case of DO stadials, with circulation slowdowns and subsequent changes remaining more limited during DO stadials than Heinrich stadials. |
author2 |
Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS) Paléocéanographie (PALEOCEAN) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS) Laboratoire de Géologie de Lyon - Terre, Planètes, Environnement Lyon (LGL-TPE) École normale supérieure - Lyon (ENS Lyon)-Université Claude Bernard Lyon 1 (UCBL) Université de Lyon-Université de Lyon-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS) Extrèmes : Statistiques, Impacts et Régionalisation (ESTIMR) Oeschger Centre for Climate Change Research (OCCR) University of Bern Bjreknes Centre for Climate Research Géochrononologie Traceurs Archéométrie (GEOTRAC) ANR-09-BLAN-0347,RETRO(2009) European Project: 339108,EC:FP7:ERC,ERC-2013-ADG,ACCLIMATE(2014) |
format |
Article in Journal/Newspaper |
author |
Waelbroeck, Claire Pichat, Sylvain Böhm, Evelyn Lougheed, Bryan C. Faranda, Davide Vrac, Mathieu Missiaen, Lise Vázquez Riveiros, Natalia Burckel, Pierre Lippold, Jörg Arz, Helge W. Dokken, Trond Thil, François Dapoigny, Arnaud |
author_facet |
Waelbroeck, Claire Pichat, Sylvain Böhm, Evelyn Lougheed, Bryan C. Faranda, Davide Vrac, Mathieu Missiaen, Lise Vázquez Riveiros, Natalia Burckel, Pierre Lippold, Jörg Arz, Helge W. Dokken, Trond Thil, François Dapoigny, Arnaud |
author_sort |
Waelbroeck, Claire |
title |
Relative timing of precipitation and ocean circulation changes in the western equatorial Atlantic over the last 45 kyr |
title_short |
Relative timing of precipitation and ocean circulation changes in the western equatorial Atlantic over the last 45 kyr |
title_full |
Relative timing of precipitation and ocean circulation changes in the western equatorial Atlantic over the last 45 kyr |
title_fullStr |
Relative timing of precipitation and ocean circulation changes in the western equatorial Atlantic over the last 45 kyr |
title_full_unstemmed |
Relative timing of precipitation and ocean circulation changes in the western equatorial Atlantic over the last 45 kyr |
title_sort |
relative timing of precipitation and ocean circulation changes in the western equatorial atlantic over the last 45 kyr |
publisher |
HAL CCSD |
publishDate |
2018 |
url |
https://hal.archives-ouvertes.fr/hal-02407248 https://hal.archives-ouvertes.fr/hal-02407248/document https://hal.archives-ouvertes.fr/hal-02407248/file/cp-14-1315-2018.pdf https://doi.org/10.5194/cp-14-1315-2018 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Greenland North Atlantic |
genre_facet |
Greenland North Atlantic |
op_source |
ISSN: 1814-9324 EISSN: 1814-9332 Climate of the Past https://hal.archives-ouvertes.fr/hal-02407248 Climate of the Past, European Geosciences Union (EGU), 2018, 14 (9), pp.1315-1330. ⟨10.5194/cp-14-1315-2018⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.5194/cp-14-1315-2018 info:eu-repo/grantAgreement/EC/FP7/339108/EU/Elucidating the Causes and Effects of Atlantic Circulation Changes through Model-Data Integration/ACCLIMATE hal-02407248 https://hal.archives-ouvertes.fr/hal-02407248 https://hal.archives-ouvertes.fr/hal-02407248/document https://hal.archives-ouvertes.fr/hal-02407248/file/cp-14-1315-2018.pdf doi:10.5194/cp-14-1315-2018 WOS: 000444984800001 |
op_rights |
http://creativecommons.org/licenses/by-nc/ info:eu-repo/semantics/OpenAccess |
op_rightsnorm |
CC-BY-NC |
op_doi |
https://doi.org/10.5194/cp-14-1315-2018 |
container_title |
Climate of the Past |
container_volume |
14 |
container_issue |
9 |
container_start_page |
1315 |
op_container_end_page |
1330 |
_version_ |
1766016995950592000 |
spelling |
ftunivnantes:oai:HAL:hal-02407248v1 2023-05-15T16:27:36+02:00 Relative timing of precipitation and ocean circulation changes in the western equatorial Atlantic over the last 45 kyr Waelbroeck, Claire Pichat, Sylvain Böhm, Evelyn Lougheed, Bryan C. Faranda, Davide Vrac, Mathieu Missiaen, Lise Vázquez Riveiros, Natalia Burckel, Pierre Lippold, Jörg Arz, Helge W. Dokken, Trond Thil, François Dapoigny, Arnaud Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS) Paléocéanographie (PALEOCEAN) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS) Laboratoire de Géologie de Lyon - Terre, Planètes, Environnement Lyon (LGL-TPE) École normale supérieure - Lyon (ENS Lyon)-Université Claude Bernard Lyon 1 (UCBL) Université de Lyon-Université de Lyon-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS) Extrèmes : Statistiques, Impacts et Régionalisation (ESTIMR) Oeschger Centre for Climate Change Research (OCCR) University of Bern Bjreknes Centre for Climate Research Géochrononologie Traceurs Archéométrie (GEOTRAC) ANR-09-BLAN-0347,RETRO(2009) European Project: 339108,EC:FP7:ERC,ERC-2013-ADG,ACCLIMATE(2014) 2018 https://hal.archives-ouvertes.fr/hal-02407248 https://hal.archives-ouvertes.fr/hal-02407248/document https://hal.archives-ouvertes.fr/hal-02407248/file/cp-14-1315-2018.pdf https://doi.org/10.5194/cp-14-1315-2018 en eng HAL CCSD European Geosciences Union (EGU) info:eu-repo/semantics/altIdentifier/doi/10.5194/cp-14-1315-2018 info:eu-repo/grantAgreement/EC/FP7/339108/EU/Elucidating the Causes and Effects of Atlantic Circulation Changes through Model-Data Integration/ACCLIMATE hal-02407248 https://hal.archives-ouvertes.fr/hal-02407248 https://hal.archives-ouvertes.fr/hal-02407248/document https://hal.archives-ouvertes.fr/hal-02407248/file/cp-14-1315-2018.pdf doi:10.5194/cp-14-1315-2018 WOS: 000444984800001 http://creativecommons.org/licenses/by-nc/ info:eu-repo/semantics/OpenAccess CC-BY-NC ISSN: 1814-9324 EISSN: 1814-9332 Climate of the Past https://hal.archives-ouvertes.fr/hal-02407248 Climate of the Past, European Geosciences Union (EGU), 2018, 14 (9), pp.1315-1330. ⟨10.5194/cp-14-1315-2018⟩ Panoply [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology info:eu-repo/semantics/article Journal articles 2018 ftunivnantes https://doi.org/10.5194/cp-14-1315-2018 2022-10-18T23:41:17Z International audience Thanks to its optimal location on the northern Brazilian margin, core MD09-3257 records both ocean circulation and atmospheric changes. The latter occur locally in the form of increased rainfall on the adjacent continent during the cold intervals recorded in Greenland ice and northern North Atlantic sediment cores (i.e., Greenland stadi-als). These rainfall events are recorded in MD09-3257 as peaks in ln(Ti / Ca). New sedimentary Pa / Th data indicate that mid-depth western equatorial water mass transport decreased during all of the Greenland stadials of the last 40 kyr. Using cross-wavelet transforms and spectrogram analysis, we assess the relative phase between the MD09-3257 sed-imentary Pa / Th and ln(Ti / Ca) signals. We show that decreased water mass transport between a depth of ∼ 1300 and 2300 m in the western equatorial Atlantic preceded increased rainfall over the adjacent continent by 120 to 400 yr at Dansgaard-Oeschger (D-O) frequencies, and by 280 to 980 yr at Heinrich-like frequencies. We suggest that the large lead of ocean circulation changes with respect to changes in tropical South American precipitation at Heinrich-like frequencies is related to the effect of a positive feedback involving iceberg discharges in the North Atlantic. In contrast, the absence of widespread ice rafted detrital layers in North Atlantic cores during DO stadials supports the hypothesis that a feedback such as this was not triggered in the case of DO stadials, with circulation slowdowns and subsequent changes remaining more limited during DO stadials than Heinrich stadials. Article in Journal/Newspaper Greenland North Atlantic Université de Nantes: HAL-UNIV-NANTES Greenland Climate of the Past 14 9 1315 1330 |