Expression of the bipolar see-saw in Antarctic climate records during the last deglaciation (Articolo in rivista)

Type

• Prodotto della ricerca (Classe)
• Articolo in rivista (Classe)

Label

• Expression of the bipolar see-saw in Antarctic climate records during the last deglaciation (Articolo in rivista) (literal)

Anno

• 2011-01-01T00:00:00+01:00 (literal)

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi

• 10.1038/ngeo1026 (literal)

Alternative label

• Stenni B.; Buiron D.; Frezzotti M.; Albani S.; Barbante C.; Bard E.; Barnola J.M.; Baroni M.; Baumgartner M.; Bonazza M.; Capron E.; Castellano E.; Chappellaz J.; Delmonte B.; Falourd S.; Genoni L.; Iacumin P.; Jouzel J.; Kipfstuhl S.; Landais A.; Lemieux-Dudon B.; Maggi V.; Masson-Delmotte V.; Mazzola C.; Minster B.; Montagnat M.; Mulvaney R.; Narcisi B.; Oerter H.; Parrenin F.; Petit J.R.; Ritz C.; Scarchilli C.; Schilt A.; Schupbach S.; Schwander J.; Selmo E.; Severi M.; Stocker T.F.; Udisti R. (2011)
  Expression of the bipolar see-saw in Antarctic climate records during the last deglaciation
  in Nature geoscience (print)
  (literal)

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori

• Stenni B.; Buiron D.; Frezzotti M.; Albani S.; Barbante C.; Bard E.; Barnola J.M.; Baroni M.; Baumgartner M.; Bonazza M.; Capron E.; Castellano E.; Chappellaz J.; Delmonte B.; Falourd S.; Genoni L.; Iacumin P.; Jouzel J.; Kipfstuhl S.; Landais A.; Lemieux-Dudon B.; Maggi V.; Masson-Delmotte V.; Mazzola C.; Minster B.; Montagnat M.; Mulvaney R.; Narcisi B.; Oerter H.; Parrenin F.; Petit J.R.; Ritz C.; Scarchilli C.; Schilt A.; Schupbach S.; Schwander J.; Selmo E.; Severi M.; Stocker T.F.; Udisti R. (literal)

Pagina inizio

• 46 (literal)

Pagina fine

• 49 (literal)

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#url

• http://www.scopus.com/inward/record.url?eid=2-s2.0-78650555903&partnerID=q2rCbXpz (literal)

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume

• 4 (literal)

Rivista

• Nature geoscience (Rivista)

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroFascicolo

• 1 (literal)

Note

• Scopu (literal)

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni

• Department of Geosciences, University of Trieste, 34127 Trieste, Italy; Laboratoire de Glaciologie et de Géophysique de l'Environnement, CNRS-Université Joseph Fourier - Grenoble, 38402 Saint Martin d'Hères Cedex, France; ENEA, CR Casaccia, 00123, Roma, Italy; Environmental Sciences Department, University of Milano Bicocca, 20126 Milano, Italy; Department of Environmental Sciences, University Cà Foscari of Venice, IDPA-CNR, 30123 Venezia, Italy; CEREGE, University Aix-Marseille, Collège de France, Europôle de l'Arbois, BP80, 13545 Aix-en-Provence cédex 4, France; Climate and Environmental Physics, Physics Institute, University of Bern, 3012 Bern, Switzerland; Laboratoire des Sciences du Climat et de l'Environnement, IPSL/CEA-CNRS-UVSQ UMR 8212, CEA Saclay, 91191 Gif-sur-Yvette cédex, France; Department of Chemistry, University of Firenze, 50019 Sesto Fiorentino, Italy; Department of Earth Sciences, University of Parma, 43100 Parma, Italy; Alfred-Wegener-Institute for Polar and Marine Research, 27568 Bremerhaven, Germany; British Antarctic Survey, NERC, Cambridge, CB3 0ET, United Kingdom (literal)

Titolo

• Expression of the bipolar see-saw in Antarctic climate records during the last deglaciation (literal)

Abstract

• Ice-core records of climate from Greenland and Antarctica show asynchronous temperature variations on millennial timescales during the last glacial period. The warming during the transition from glacial to interglacial conditions was markedly different between the hemispheres, a pattern attributed to the thermal bipolar see-saw. However, a record from the Ross Sea sector of East Antarctica has been suggested to be synchronous with Northern Hemisphere climate change. Here we present a temperature record from the Talos Dome ice core, also located in the Ross Sea sector. We compare our record with ice-core analyses from Greenland, based on methane synchronization, and find clearly asynchronous temperature changes during the deglaciation. We also find distinct differences in Antarctic records, pointing to differences in the climate evolution of the Indo-Pacific and Atlantic sectors of Antarctica. In the Atlantic sector, we find that the rate of warming slowed between 16,000 and 14,500 years ago, parallel with the deceleration of the rise in atmospheric carbon dioxide concentrations and with a slight cooling over Greenland. In addition, our chronology supports the hypothesis that the cooling of the Antarctic Cold Reversal is synchronous with the Bølling-Allerød warming in the northern hemisphere 14,700 years ago. © 2011 Macmillan Publishers Limited. All rights reserved. (literal)

Prodotto di

• Ambiente e clima: processi, cambiamenti globali e contaminazione chimica in aree polari, remote e antropizzate (TA.P02.024.001) (Modulo)
• Institute for the Dynamics of Environmental Processes (IDPA) (Istituto)

Autore CNR

• CARLO BARBANTE (Persona)

Incoming links:

Prodotto

• Institute for the Dynamics of Environmental Processes (IDPA) (Istituto)
• Ambiente e clima: processi, cambiamenti globali e contaminazione chimica in aree polari, remote e antropizzate (TA.P02.024.001) (Modulo)

Autore CNR di

• CARLO BARBANTE (Persona)

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#rivistaDi

• Nature geoscience (Rivista)