globalchange  > 影响、适应和脆弱性
DOI: 10.1007/s00531-014-1042-5
Scopus记录号: 2-s2.0-84906303932
论文题名:
Spatial-temporal differences in climate change at different altitudes, northeastern Qinghai-Tibetan Plateau during the Holocene period
作者: Liu B.; Jin H.; Sun L.; Su Z.; Sun Z.; Zhao S.; Miao Y.
刊名: International Journal of Earth Sciences
ISSN: 14373254
出版年: 2014
卷: 103, 期:6
起始页码: 1699
结束页码: 1710
语种: 英语
英文关键词: Climate change ; Different altitudes ; Gonghe Basin ; Holocene ; Spatial-temporal differences
Scopus关键词: climate feedback ; climate variation ; Holocene ; paleoclimate ; reconstruction ; spatiotemporal analysis ; topographic effect ; China ; Gonghe Basin ; Qinghai ; Qinghai-Xizang Plateau
英文摘要: The history of climate change and related driving mechanisms of the Gonghe Basin, northeastern Qinghai-Tibetan Plateau, China, was reconstructed in the Holocene epoch, based on the comprehensive analysis of multi-proxies consisting of magnetic susceptibility, grain size, and geochemical elements from eolian and peat deposits at different altitudes. The results indicate that Holocene climate change at different altitudes is both consistent and different: a synchronous record of an increased warm-humid phase (10.0-8.5 ka) and a cold phase around 8.2 ka in the Early Holocene; an optimal warm-humid condition in marginal mountains of the Gonghe Basin in the Mid-Holocene; and a gradual decline in temperature and humidity in the Late Holocene. The Gonghe Basin interior in the Mid-Holocene was relatively arid, with increased moisture in the Late Holocene. On this basis, we compared our results to the paleoclimatic record in the low-latitude Asian monsoonal region, which indicates that, in addition to the Asian summer monsoonal strength having influenced regional climate change, the upward and subsidence motion of airflow over the Qinghai-Tibetan Plateau induced by topographic conditions, evaporation, and the feedback effect by the substrate was also influential. The latter was especially important for spatial-temporal differences in Middle and Late Holocene climatic changes at different altitudes. © 2014 Springer-Verlag Berlin Heidelberg.
URL: https://www.scopus.com/inward/record.uri?eid=2-s2.0-84906303932&doi=10.1007%2fs00531-014-1042-5&partnerID=40&md5=39d1267e9da3557be7a91c10c4dedd97
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/70382
Appears in Collections:影响、适应和脆弱性
气候减缓与适应

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作者单位: Key Laboratory of Desert and Desertification, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou, 730000, China; School of History and Culture, Shanxi University, Taiyuan, 030006 Shanxi, China; Key Laboratory of Western China Environmental System (Ministry of Education), Lanzhou University, Lanzhou, 730000, China

Recommended Citation:
Liu B.,Jin H.,Sun L.,et al. Spatial-temporal differences in climate change at different altitudes, northeastern Qinghai-Tibetan Plateau during the Holocene period[J]. International Journal of Earth Sciences,2014-01-01,103(6)
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