Khodri Myriam, Izumo Takeshi, Vialard Jérôme, Janicot Serge, Cassou Christophe, Lengaigne Matthieu, Mignot Juliette, Gastineau Guillaume, Guilyardi Eric, Lebas Nicolas, Robock Alan, McPhaden Michael J
Laboratoire d'Océanographie et du Climat: Expérimentations et approches numériques, Sorbonne Universités, UPMC Université Paris 06, IPSL, UMR CNRS/IRD/MNHN, F-75005, Paris, France.
Indo-French Cell for Water Sciences, IISc-NIO-IITM-IRD Joint International Laboratory, NIO, 403002, Goa, India.
Nat Commun. 2018 Feb 22;9(1):855. doi: 10.1038/s41467-018-03365-y.
The original version of this Article omitted a reference to previous work in 'Mann, M.E., Cane, M.A., Zebiak, S.E., Clement, A., Volcanic and Solar Forcing of the Tropical Pacific Over the Past 1000 Years, J. Climate 18, 447-456 (2005)'. This has been added as reference 62 at the end of the fourth sentence of the fourth paragraph of the Introduction: 'Early studies using simple coupled ocean-atmosphere models proposed that following volcano-induced surface cooling, upwelling in the eastern equatorial Pacific acting on a reduced vertical temperature contrast between the ocean surface and interior leads to anomalous warming in this region, thereby favouring El Niño development the following year.' This has been corrected in the PDF and HTML versions of the Article.
本文的原始版本遗漏了对先前研究“Mann, M.E., Cane, M.A., Zebiak, S.E., Clement, A., 《过去1000年热带太平洋的火山和太阳强迫》，《气候杂志》18卷，第447 - 456页（2005年）”的引用。现已在引言第四段第四句末尾添加此引用作为参考文献62：“早期使用简单耦合海洋 - 大气模型的研究表明，在火山引起的表面冷却之后，赤道东太平洋的上升流作用于海洋表面和内部之间减小的垂直温度差异，导致该区域出现异常变暖，从而有利于次年厄尔尼诺现象的发展。”本文的PDF和HTML版本已对此进行了修正。
