IOCAS-IR  > 深海极端环境与生命过程研究中心
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
ISSN1040-6182
卷号679页码:36-42
通讯作者Jin, Zhangdong(zhdjin@ieecas.cn)
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
DOI10.1016/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.
条目包含的文件
条目无相关文件。
个性服务
推荐该条目
保存到收藏夹
查看访问统计
导出为Endnote文件
谷歌学术
谷歌学术中相似的文章
[Zhang, Run]的文章
[Feng, Qi]的文章
[Zhang, Fei]的文章
百度学术
百度学术中相似的文章
[Zhang, Run]的文章
[Feng, Qi]的文章
[Zhang, Fei]的文章
必应学术
必应学术中相似的文章
[Zhang, Run]的文章
[Feng, Qi]的文章
[Zhang, Fei]的文章
相关权益政策
暂无数据
收藏/分享
所有评论 (0)
暂无评论
 

除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。