| Correspondence between the ENSO-like state and glacial-interglacial condition during the past 360 kyr | |
Zhang Shuai1,3 ; Li Tiegang2,4; Chang Fengming1,4; Yu Zhoufei1,2; Xiong Zhifang1; Wang Haixia5
| |
| 2017-09-01 | |
| 发表期刊 | CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY
 |
| 卷号 | 35期号:5页码:1018-1031 |
| 文章类型 | Article |
| 摘要 | In the warming world, tropical Pacific sea surface temperature (SST) variation has received considerable attention because of its enormous influence on global climate change, particularly the El Nio-Southern Oscillation process. Here, we provide new high-resolution proxy records of the magnesium/calcium ratio and the oxygen isotope in foraminifera from a core on the Ontong-Java Plateau to reconstruct the SST and hydrological variation in the center of the Western Pacific Warm Pool (WPWP) over the last 360 000 years. In comparison with other Mg/Ca-derived SST and delta O-18 records, the results suggested that in a relatively stable condition, e.g., the last glacial maximum (LGM) and other glacial periods, the tropical Pacific would adopt a La Nia-like state, and the Walker and Hadley cycles would be synchronously enhanced. Conversely, El Nio-like conditions could have occurred in the tropical Pacific during fastchanging periods, e.g., the termination and rapidly cooling stages of interglacial periods. In the light of the sensitivity of the Eastern Pacific Cold Tongue (EPCT) and the inertia of the WPWP, we hypothesize an inter-restricted relationship between the WPWP and EPCT, which could control the zonal gradient variation of SST and affect climate change. |
| 关键词 | Western Pacific Warm Pool (Wpwp) Sea Surface Temperature (Sst) El Nino-southern Oscillation (Enso) |
| DOI | 10.1007/s00343-017-6082-9 |
| 收录类别 | SCI |
| 语种 | 英语 |
| WOS记录号 | WOS:000410093300004 |
| 引用统计 | |
| 文献类型 | 期刊论文 |
| 版本 | 出版稿 |
| 条目标识符 | http://ir.qdio.ac.cn/handle/337002/143179 |
| 专题 | 海洋地质与环境重点实验室 |
| 作者单位 | 1.Chinese Acad Sci, Inst Oceanol, Key Lab Marine Geol & Environm, Qingdao 266071, Peoples R China 2.SOA, Key Lab Marine Sedimentol & Environm Geol, Inst Oceanog 1, Qingdao 266061, Peoples R China 3.Univ Chinese Acad Sci, Beijing 100049, Peoples R China 4.Qingdao Natl Lab Marine Sci & Technol, Lab Marine Geol, Qingdao 266061, Peoples R China 5.Ningbo City Land Resources Bur Yinzhou Branch, Ningbo 315100, Zhejiang, Peoples R China |
| 第一作者单位 | 中国科学院海洋研究所 |
| 推荐引用方式 GB/T 7714 | Zhang Shuai,Li Tiegang,Chang Fengming,et al. Correspondence between the ENSO-like state and glacial-interglacial condition during the past 360 kyr[J]. CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY,2017,35(5):1018-1031. |
| APA | Zhang Shuai,Li Tiegang,Chang Fengming,Yu Zhoufei,Xiong Zhifang,&Wang Haixia.(2017).Correspondence between the ENSO-like state and glacial-interglacial condition during the past 360 kyr.CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY,35(5),1018-1031. |
| MLA | Zhang Shuai,et al."Correspondence between the ENSO-like state and glacial-interglacial condition during the past 360 kyr".CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY 35.5(2017):1018-1031. |
| 条目包含的文件 | ||||||
| 文件名称/大小 | 文献类型 | 版本类型 | 开放类型 | 使用许可 | ||
| Correspondence betwe（2085KB） | 期刊论文 | 出版稿 | 限制开放 | CC BY-NC-SA | 浏览 | |
除非特别说明，本系统中所有内容都受版权保护，并保留所有权利。
修改评论