Direct north-south synchroniszation of abrupt climate change record in ice cores using Beryllium 10
| Data(s) |
2007
|
|---|---|
| Resumo |
A new, decadally resolved record of the 10Be peak at 41 kyr from the EPICA Dome C ice core (Antarctica) is used to match it with the same peak in the GRIP ice core (Greenland). This permits a direct synchronisation of the climatic variations around this time period, independent of uncertainties related to the ice age-gas age difference in ice cores. Dansgaard-Oeschger event 10 is in the period of best synchronisation and is found to be coeval with an Antarctic temperature maximum. Simulations using a thermal bipolar seesaw model agree reasonably well with the observed relative climate chronology in these two cores. They also reproduce three Antarctic warming events observed between A1 and A2. |
| Formato |
application/pdf |
| Identificador |
http://boris.unibe.ch/25263/1/cp-3-541-2007.pdf Raisbeck, G.M.; Yiou, F.; Jouzel, J.; Stocker, Thomas (2007). Direct north-south synchroniszation of abrupt climate change record in ice cores using Beryllium 10. Climate of the past, 3(3), pp. 541-547. Göttingen: Copernicus Publications 10.5194/cp-3-541-2007 <http://dx.doi.org/10.5194/cp-3-541-2007> doi:10.7892/boris.25263 info:doi:10.5194/cp-3-541-2007 urn:issn:1814-9324 |
| Idioma(s) |
eng |
| Publicador |
Copernicus Publications |
| Relação |
http://boris.unibe.ch/25263/ |
| Direitos |
info:eu-repo/semantics/openAccess |
| Fonte |
Raisbeck, G.M.; Yiou, F.; Jouzel, J.; Stocker, Thomas (2007). Direct north-south synchroniszation of abrupt climate change record in ice cores using Beryllium 10. Climate of the past, 3(3), pp. 541-547. Göttingen: Copernicus Publications 10.5194/cp-3-541-2007 <http://dx.doi.org/10.5194/cp-3-541-2007> |
| Tipo |
info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion PeerReviewed |
