Articles | Volume 13, issue 6
https://doi.org/10.5194/cp-13-729-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/cp-13-729-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
30 Jun 2017
Research article |
| 30 Jun 2017
Regional seesaw between the North Atlantic and Nordic Seas during the last glacial abrupt climate events
UMR 5805, EPOC (Environnements et Paléoenvironnements
Océaniques et Continentaux), CNRS-EPHE-Université de Bordeaux, 33615
Pessac, France
Frédérique Eynaud
UMR 5805, EPOC (Environnements et Paléoenvironnements
Océaniques et Continentaux), CNRS-EPHE-Université de Bordeaux, 33615
Pessac, France
Didier Swingedouw
UMR 5805, EPOC (Environnements et Paléoenvironnements
Océaniques et Continentaux), CNRS-EPHE-Université de Bordeaux, 33615
Pessac, France
Valérie Masson-Delmotte
UMR8212, LSCE (Laboratoire des Sciences du Climat et de
l'Environnement)/IPSL (Institut Pierre Simon Laplace), CEA/CNRS-INSU/UVSQ,
91191 Gif-sur-Yvette CEDEX, France
Jens Matthiessen
AWI (Alfred Wegener Institute), Helmholtz Centre for Polar and Marine
Research, 27568 Bremerhaven, Germany
Catherine Kissel
UMR8212, LSCE (Laboratoire des Sciences du Climat et de
l'Environnement)/IPSL (Institut Pierre Simon Laplace), CEA/CNRS-INSU/UVSQ,
91191 Gif-sur-Yvette CEDEX, France
Jena Zumaque
UMR 5805, EPOC (Environnements et Paléoenvironnements
Océaniques et Continentaux), CNRS-EPHE-Université de Bordeaux, 33615
Pessac, France
now at: GEOTOP, UQAM, Montréal, Québec H3C 3P8, Canada
Linda Rossignol
UMR 5805, EPOC (Environnements et Paléoenvironnements
Océaniques et Continentaux), CNRS-EPHE-Université de Bordeaux, 33615
Pessac, France
Jean Jouzel
UMR8212, LSCE (Laboratoire des Sciences du Climat et de
l'Environnement)/IPSL (Institut Pierre Simon Laplace), CEA/CNRS-INSU/UVSQ,
91191 Gif-sur-Yvette CEDEX, France
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Cited
10 citations as recorded by crossref.
- Marine Isotope Stage 4 (71–57 ka) on the Western European margin: Insights to the drainage and dynamics of the Western European Ice Sheet S. Toucanne et al. 10.1016/j.gloplacha.2023.104221
- Rapid reductions and millennial-scale variability in Nordic Seas sea ice cover during abrupt glacial climate changes H. Sadatzki et al. 10.1073/pnas.2005849117
- Diatom-reconstructed summer sea-surface temperatures and climatic events off North Iceland during the last deglaciation and Holocene L. Sha et al. 10.1016/j.palaeo.2022.111154
- Spatio-temporal dynamics of hydrographic reorganizations and iceberg discharges at the junction between the Northeast Atlantic and Norwegian Sea basins surrounding Heinrich event 4 M. Wary et al. 10.1016/j.epsl.2017.10.042
- Consistent fluctuations in intermediate water temperature off the coast of Greenland and Norway during Dansgaard-Oeschger events E. Sessford et al. 10.1016/j.quascirev.2019.105887
- The North Atlantic Glacial Eastern Boundary Current as a Key Driver for Ice‐Sheet—AMOC Interactions and Climate Instability S. Toucanne et al. 10.1029/2020PA004068
- Dinoflagellate fossils: Geological and biological applications A. Penaud et al. 10.1016/j.revmic.2018.09.003
- Circulation adjustment in the Arctic and Atlantic in response to Greenland and Antarctic mass loss J. Berk et al. 10.1007/s00382-021-05755-3
- Are Past Sea-Ice Reconstructions Based on Planktonic Foraminifera Realistic? Study of the Last 50 ka as a Test to Validate Reconstructed Paleohydrography Derived from Transfer Functions Applied to Their Fossil Assemblages F. Eynaud et al. 10.3390/geosciences11100409
- Consistently dated Atlantic sediment cores over the last 40 thousand years C. Waelbroeck et al. 10.1038/s41597-019-0173-8
10 citations as recorded by crossref.
- Marine Isotope Stage 4 (71–57 ka) on the Western European margin: Insights to the drainage and dynamics of the Western European Ice Sheet S. Toucanne et al. 10.1016/j.gloplacha.2023.104221
- Rapid reductions and millennial-scale variability in Nordic Seas sea ice cover during abrupt glacial climate changes H. Sadatzki et al. 10.1073/pnas.2005849117
- Diatom-reconstructed summer sea-surface temperatures and climatic events off North Iceland during the last deglaciation and Holocene L. Sha et al. 10.1016/j.palaeo.2022.111154
- Spatio-temporal dynamics of hydrographic reorganizations and iceberg discharges at the junction between the Northeast Atlantic and Norwegian Sea basins surrounding Heinrich event 4 M. Wary et al. 10.1016/j.epsl.2017.10.042
- Consistent fluctuations in intermediate water temperature off the coast of Greenland and Norway during Dansgaard-Oeschger events E. Sessford et al. 10.1016/j.quascirev.2019.105887
- The North Atlantic Glacial Eastern Boundary Current as a Key Driver for Ice‐Sheet—AMOC Interactions and Climate Instability S. Toucanne et al. 10.1029/2020PA004068
- Dinoflagellate fossils: Geological and biological applications A. Penaud et al. 10.1016/j.revmic.2018.09.003
- Circulation adjustment in the Arctic and Atlantic in response to Greenland and Antarctic mass loss J. Berk et al. 10.1007/s00382-021-05755-3
- Are Past Sea-Ice Reconstructions Based on Planktonic Foraminifera Realistic? Study of the Last 50 ka as a Test to Validate Reconstructed Paleohydrography Derived from Transfer Functions Applied to Their Fossil Assemblages F. Eynaud et al. 10.3390/geosciences11100409
- Consistently dated Atlantic sediment cores over the last 40 thousand years C. Waelbroeck et al. 10.1038/s41597-019-0173-8
Latest update: 19 Apr 2024
Short summary
The last glacial period was punctuated by abrupt climatic variations, whose cold atmospheric phases have been commonly associated with cold sea-surface temperatures and expansion of sea ice in the North Atlantic and adjacent seas. Here we provide direct evidence of a regional paradoxical see-saw pattern: cold Greenland and North Atlantic phases coincide with warmer sea-surface conditions and shorter seasonal sea-ice cover durations in the Norwegian Sea as compared to warm phases.
The last glacial period was punctuated by abrupt climatic variations, whose cold atmospheric...
