Knowledge Management System Of Institute of Oceanology, Chinese Academy of Sciences
Fluctuations of Qiangyong glacier in southern Tibetan Plateau over the past 500 years recorded by proglacial lacustrine sediments | |
Zhang, Run1,2; Feng, Qi2,5; Zhang, Fei2; Li, Le3; Xu, Yang2; Jin, Zhangdong2,4 | |
2024-01-10 | |
发表期刊 | QUATERNARY INTERNATIONAL |
ISSN | 1040-6182 |
卷号 | 679页码:36-42 |
通讯作者 | Jin, Zhangdong([email protected]) |
摘要 | The glaciers of the Tibetan Plateau have undergone profound changes due to rapid global warming, but the nature of their response to climate change at various settings remains unclear. This study focuses on the analysis (grain sizes, magnetic susceptibility, and element ratios) of a sedimentary core from a proglacial lake (Qiangyong (QY) Co) at the southern Tibetan Plateau, based upon the 210Pb and 137Cs dating, aiming to unveil the fluctu-ations of the QY glacier over the recent 500 years and its response to global warming. Four pre-1900s distinct glacier advance/cold intervals (C1: 1560s, C2: 1660s, C3: 1760s and C4: 1860s), a minor advance in the 1950s and an extensive glacier retreat since the 2010s were discerned. There are five glacier fluctuation cycles, each spanning approximately 100 years, correlating generally well with the Northern Hemisphere temperature pat-terns on a century time scale. The glacier advances align with the cold periods, whereas the retreats correspond to the warm intervals. However, coarse grain sizes indicated a marked glacier shrinkage of the QY glacier since the 1920s owing to global warming, over-shading the inherent 100-years fluctuation cyclic variations intrinsic to glaciers. The reason is that after QY glacier has significantly shrunk to higher altitude, the response of the glacier to climate change is no longer as sensitive as at the lower altitude, even under post-industrial-revolution warming. The QY glacier and even the entire Himalayan region will face the threat of glacier melting during the 21st century, but dynamic patterns of glacier retreats in higher Himalayan regions may differ from that in the low-altitude. |
关键词 | Proglacial lake Global warming Little Ice Age Qiangyong glacier |
DOI | 10.1016/j.quaint.2023.11.011 |
收录类别 | SCI |
语种 | 英语 |
资助项目 | National Natural Science Foundation of China[42221003]; Strategic Priority Research Program of CAS[XDB40020100] |
WOS研究方向 | Physical Geography ; Geology |
WOS类目 | Geography, Physical ; Geosciences, Multidisciplinary |
WOS记录号 | WOS:001143598800001 |
出版者 | PERGAMON-ELSEVIER SCIENCE LTD |
WOS关键词 | LATE-HOLOCENE ; CENTRAL JOTUNHEIMEN ; CLIMATE-CHANGE ; ICE-AGE ; LAKE ; NORWAY ; RECONSTRUCTION ; HIMALAYA ; CORE ; TILL |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://ir.qdio.ac.cn/handle/337002/184363 |
专题 | 深海极端环境与生命过程研究中心 |
通讯作者 | Jin, Zhangdong |
作者单位 | 1.Nanjing Univ, Dept Earth & Planetary Sci, Key Lab Surficial Geochem, Minist Educ, Nanjing 210023, Jiangsu, Peoples R China 2.Chinese Acad Sci, Inst Earth Environm, SKLLQG, Xian 710061, Shaanxi, Peoples R China 3.Chinese Acad Sci, Ctr Deep Sea Res, Inst Oceanol, Qingdao 266071, Shandong, Peoples R China 4.Xi An Jiao Tong Univ, Inst Global Environm Change, Xian 710049, Shaanxi, Peoples R China 5.Univ Chinese Acad Sci, Beijing 100049, Peoples R China |
推荐引用方式 GB/T 7714 | Zhang, Run,Feng, Qi,Zhang, Fei,et al. Fluctuations of Qiangyong glacier in southern Tibetan Plateau over the past 500 years recorded by proglacial lacustrine sediments[J]. QUATERNARY INTERNATIONAL,2024,679:36-42. |
APA | Zhang, Run,Feng, Qi,Zhang, Fei,Li, Le,Xu, Yang,&Jin, Zhangdong.(2024).Fluctuations of Qiangyong glacier in southern Tibetan Plateau over the past 500 years recorded by proglacial lacustrine sediments.QUATERNARY INTERNATIONAL,679,36-42. |
MLA | Zhang, Run,et al."Fluctuations of Qiangyong glacier in southern Tibetan Plateau over the past 500 years recorded by proglacial lacustrine sediments".QUATERNARY INTERNATIONAL 679(2024):36-42. |
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