Decoupling of stalagmite-derived asian summer monsoon records from north atlantic temperature change during marine oxygen isotope stage 5d
文献类型：期刊论文
| 作者 | Zhou, Houyun1; Zhao, Jianxin2; Zhang, Pingzhong3; Shen, Chuan-Chou4; Chi, Baoquan1,5; Feng, Yuexing2; Lin, Yin4; Guan, Huazheng1,5; You, Chen-Feng6 |
| 刊名 | Quaternary research
 |
| 出版日期 | 2008-09-01 |
| 卷号 | 70期号:2页码:315-321 |
| 关键词 | Asian monsoon north atlantic Stalagmite Paleoclimate Millennial-scale event Decoupling Teleconnection Marine oxygen isotope stage 5d |
| ISSN号 | 0033-5894 |
| DOI | 10.1016/j.yqres.2008.04.007 |
| 通讯作者 | Zhou, houyun(hyzhou@gig.ac.cn) |
| 英文摘要 | The asian monsoon is an important component of the global climate system. seasonal variations in wind, rainfall, and temperature associated with the asian monsoon systems affect a vast expanse of tropical and subtropical asia. speleothem-derived summer monsoon variation ill east asia was previously found to be closely associated with millennial-scale change in temperature in the north atlantic region between 75 and 10 ka. new evidence recovered from east asia, however, suggests that the teleconnection between summer monsoon ill east asia and temperature change in the north atlantic region may have significantly reduced during 120 to - 110 ka, a period directly after the full last interglaciation and corresponding roughly to marine oxygen isotope stage 5d. this reduction may be due to the low ice volume in the north hemisphere at that time, which makes the millennial-scale change in temperature in the north atlantic region less effective in influencing the asian summer monsoon. this is important for investigating the mechanisms controlling the asian summer monsoon and the paleoclimatic teleconnection between east asia and the north atlantic region, and for predicting monsoon-associated precipitation in east asia under a global-warming trend. (c) 2008 university of washington. all rights reserved. |
| WOS关键词 | ICE CORE PROJECT ; HIGH-RESOLUTION ; GREENLAND ICE ; CENTRAL CHINA ; DONGGE CAVE ; DELTA O-18 ; CLIMATE ; HOLOCENE ; EVENTS ; INSTABILITY |
| WOS研究方向 | Physical Geography ; Geology |
| WOS类目 | Geography, Physical ; Geosciences, Multidisciplinary |
| 语种 | 英语 |
| WOS记录号 | WOS:000259157500016 |
| 出版者 | ACADEMIC PRESS INC ELSEVIER SCIENCE |
| URI标识 | http://www.irgrid.ac.cn/handle/1471x/2384166 |
| 专题 | 中国科学院大学 |
| 通讯作者 | Zhou, Houyun |
| 作者单位 | 1.Chinese Acad Sci, Guangzhou Inst Geochem, Guangzhou 510640, Guangdong Prov, Peoples R China 2.Univ Queensland, Ctr Microscopy & Microanal, Radiogen Isotope Lab, Brisbane, Qld 4072, Australia 3.Lanzhou Univ, Coll Earth & Environm Sci, Key Lab Western Chinas Environm Syst Minist Educ, Lanzhou 730000, Peoples R China 4.Natl Taiwan Univ, Dept Geosci, Taipei 106, Taiwan 5.Chinese Acad Sci, Grad Sch, Beijing 100039, Peoples R China 6.Natl Cheng Kung Univ, Earth Dynam Syst Res Ctr, Tainan 701, Taiwan |
| 推荐引用方式 GB/T 7714 | Zhou, Houyun,Zhao, Jianxin,Zhang, Pingzhong,et al. Decoupling of stalagmite-derived asian summer monsoon records from north atlantic temperature change during marine oxygen isotope stage 5d[J]. Quaternary research,2008,70(2):315-321. |
| APA | Zhou, Houyun.,Zhao, Jianxin.,Zhang, Pingzhong.,Shen, Chuan-Chou.,Chi, Baoquan.,...&You, Chen-Feng.(2008).Decoupling of stalagmite-derived asian summer monsoon records from north atlantic temperature change during marine oxygen isotope stage 5d.Quaternary research,70(2),315-321. |
| MLA | Zhou, Houyun,et al."Decoupling of stalagmite-derived asian summer monsoon records from north atlantic temperature change during marine oxygen isotope stage 5d".Quaternary research 70.2(2008):315-321. |
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来源：中国科学院大学
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