globalchange  > 影响、适应和脆弱性
DOI: 10.1007/s00531-013-0896-2
论文题名:
Holocene lake level variations on the Qinghai-Tibetan Plateau
作者: Liu X.-J.; Lai Z.-P.; Zeng F.-M.; Madsen D.B.; E C.-Y.
刊名: International Journal of Earth Sciences
出版年: 2013
卷: 102, 期:7
起始页码: 2007
结束页码: 2016
语种: 英语
英文关键词: Holocene lake level variations ; Paleoshorelines ; Qinghai-Tibetan Plateau (QTP)
Scopus关键词: chronology ; coastal evolution ; highstand ; Holocene ; lake level ; paleoenvironment ; satellite imagery ; shoreline change ; China ; Gangdise Mountains ; Qinghai-Xizang Plateau ; Xizang
英文摘要: Paleoshorelines indicative of multiple high lake stages can be found around many lakes on the Qinghai-Tibetan Plateau (QTP). Conspicuous paleoshorelines associated with the most recent highstands can be readily observed on satellite images and during field investigations. However, earlier paleoshorelines have been identified at only a few sites around these lakes due to a lack of clear shoreline features and limited spatial extension of those that can be identified. We investigated past lake highstands using published chronologies, Aster-DEM, Google Earth, and ArcGIS 9.2 software. These data suggest that (1) paleoshorelines of the most recent lake highstand were formed during the Holocene; (2) during this highstand, lake levels reached more than 90, 60-90, and 30-60 m higher than present in the central Gangdise and western Qiangtang areas, while in the eastern Qiangtang, Holxil-Yushu, and northeastern QTP areas highstands did not exceed 30 m above modern; (3) during the early Holocene, some lakes on the southwestern QTP combined to form large lakes, while lakes in the inland areas of the QTP were only a little larger during the Holocene high lake level stages. © 2013 Springer-Verlag Berlin Heidelberg.
URL: https://www.scopus.com/inward/record.uri?eid=2-s2.0-84884418271&doi=10.1007%2fs00531-013-0896-2&partnerID=40&md5=0c89fa2502cf7eebb4e44cbb317a6800
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/70504
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 Salt Lake Resources and Chemistry, Qinghai Institute of Salt Lakes, Chinese Academy of Sciences, Xining, 810008, China; Key Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, 100085, China; School of Life and Geographic Science, Qinghai Normal University, Wusi Road, Xining, China; MOE Key Laboratory of West China's Environmental System, Research School of Arid Environment and Climate Change, Lanzhou University, Lanzhou, 730000, China

Recommended Citation:
Liu X.-J.,Lai Z.-P.,Zeng F.-M.,et al. Holocene lake level variations on the Qinghai-Tibetan Plateau[J]. International Journal of Earth Sciences,2013-01-01,102(7)
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