Global S&T Development Trend Analysis Platform of Resources and Environment
DOI | 10.1007/s00382-017-3784-9 |
Lagged response of summer precipitation to insolation forcing on the northeastern Tibetan Plateau during the Holocene | |
Zhang, Xiaojian1; Jin, Liya2,3; Chen, Jie3; Lu, Huayu1; Chen, Fahu3 | |
2018-05-01 | |
发表期刊 | CLIMATE DYNAMICS |
ISSN | 0930-7575 |
EISSN | 1432-0894 |
出版年 | 2018 |
卷号 | 50页码:3117-3129 |
文章类型 | Article |
语种 | 英语 |
国家 | Peoples R China |
英文摘要 | The precipitation changes on the northeastern Tibetan Plateau during the Holocene remain unclear due to discrepancies among different proxy records. We compared proxy records with the results from a transient simulation performed using the Kiel Climate Model forced by orbital variations, to analyse summer precipitation changes in this area during the Holocene (9.5-0 ka BP). The model results suggested increasing amounts of summer precipitation from 9.5 to similar to 6.2 ka BP and a persistent decline thereafter, which matched well with pollen records but was inconsistent with ostracod delta O-18 records. The Holocene climatic optimum lagged the Northern Hemisphere summer insolation maximum by similar to 3.5 ka, caused by the interplay between the East Asian summer monsoon (EASM) circulation and the mid-latitude westerlies. The ostracod delta O-18 values reflected the strength of the EASM circulation. A strong EASM circulation increased the transport of water vapour towards the northeastern Tibetan Plateau from the northwestern Pacific. Weakened mid-latitude westerlies increased the incursion of cold air masses into the northeastern Tibetan Plateau. During the early Holocene, relatively strong mid-latitude westerlies, resulting from an enhanced Arctic Oscillation, reduced summer precipitation on the northeastern Tibetan Plateau, in spite of a strong insolation-driven EASM circulation. The weakening EASM circulation and the strengthening westerlies together induced the decreasing trend of summer precipitation from the middle to late Holocene. In addition, summer precipitation variations were further modulated by sea-surface temperatures in the northwestern Pacific, through weakening the strength of the EASM. |
英文关键词 | Holocene East Asian summer monsoon Northeastern Tibetan Plateau Model-proxy comparison Orbital forcing |
领域 | 气候变化 |
收录类别 | SCI-E |
WOS记录号 | WOS:000429650700001 |
WOS关键词 | QINGHAI LAKE AREA ; ASIAN MONSOON ; LAST DEGLACIATION ; VAPOR TRANSPORT ; OXYGEN-ISOTOPE ; CLIMATE ; CHINA ; CIRCULATION ; SEDIMENTS ; RECORDS |
WOS类目 | Meteorology & Atmospheric Sciences |
WOS研究方向 | Meteorology & Atmospheric Sciences |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://119.78.100.173/C666/handle/2XK7JSWQ/35967 |
专题 | 气候变化 |
作者单位 | 1.Nanjing Univ, Sch Geog & Oceanog Sci, Nanjing 210023, Jiangsu, Peoples R China; 2.Chengdu Univ Informat Technol, Sch Atmospher Sci, Chengdu 610225, Sichuan, Peoples R China; 3.Lanzhou Univ, Coll Earth & Environm Sci, MOE Key Lab Western Chinas Environm Syst, Lanzhou 730000, Gansu, Peoples R China |
推荐引用方式 GB/T 7714 | Zhang, Xiaojian,Jin, Liya,Chen, Jie,et al. Lagged response of summer precipitation to insolation forcing on the northeastern Tibetan Plateau during the Holocene[J]. CLIMATE DYNAMICS,2018,50:3117-3129. |
APA | Zhang, Xiaojian,Jin, Liya,Chen, Jie,Lu, Huayu,&Chen, Fahu.(2018).Lagged response of summer precipitation to insolation forcing on the northeastern Tibetan Plateau during the Holocene.CLIMATE DYNAMICS,50,3117-3129. |
MLA | Zhang, Xiaojian,et al."Lagged response of summer precipitation to insolation forcing on the northeastern Tibetan Plateau during the Holocene".CLIMATE DYNAMICS 50(2018):3117-3129. |
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