Asynchrony between Antarctic temperature and CO(2) associated with obliquity over the past 720,000 years

The δD temperature proxy in Antarctic ice cores varies in parallel with CO(2) through glacial cycles. However, these variables display a puzzling asynchrony. Well-dated records of Southern Ocean temperature will provide crucial information because the Southern Ocean is likely key in regulating CO(2)...

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Publicado en:Nat Commun
Main Authors: Uemura, Ryu, Motoyama, Hideaki, Masson-Delmotte, Valérie, Jouzel, Jean, Kawamura, Kenji, Goto-Azuma, Kumiko, Fujita, Shuji, Kuramoto, Takayuki, Hirabayashi, Motohiro, Miyake, Takayuki, Ohno, Hiroshi, Fujita, Koji, Abe-Ouchi, Ayako, Iizuka, Yoshinori, Horikawa, Shinichiro, Igarashi, Makoto, Suzuki, Keisuke, Suzuki, Toshitaka, Fujii, Yoshiyuki
Formato: Artigo
Idioma:Inglês
Publicado: Nature Publishing Group UK 2018
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Article
Acceso en liña:https://ncbi.nlm.nih.gov/pmc/articles/PMC5840396/
https://ncbi.nlm.nih.gov/pubmed/29511182
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41467-018-03328-3
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