中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Reconstruction of paleoglacial equilibrium-line altitudes during the Last Glacial Maximum in the Diancang Massif, Northwest Yunnan Province, China

文献类型:期刊论文

作者Zeng, Hongyun2,3; Li, Peng3; Zhu, Yunqiang; Zhang, Jinqu1; Zhao, Xiaoqin4
刊名OPEN GEOSCIENCES
出版日期2023-03-31
卷号15期号:1页码:20220426
ISSN号2391-5447
关键词paleoglacier equilibrium-line altitudes Last Glacial Maximum Diancang Massif paleoglacier reconstruction Tali Glacial Stage
DOI10.1515/geo-2022-0426
文献子类Article
英文摘要Equilibrium-line altitudes (ELAs) are an important proxy of the fluctuations and mass-balance characteristics of glaciers and have been widely used to reconstruct regional paleoclimatic conditions. The Diancang Massif, which has experienced the well-known Tali Glacial Stage was uplifted during MIS 3b (marine isotope stages). With its unique characteristics, the Diancang Massif has become an irreplaceable area for the study of inland paleoclimatic and paleo-environmental changes in China. Nevertheless, despite the considerable amount of glaciological studies on this area, a detailed and systematic estimation of paleoglacial ELAs during the Last Glacial Maximum remains to be performed. In this study, several approaches are employed to estimate the ELAs on the basis of previous studies. The results are compared and analyzed, and the final results are determined using a weighted arithmetic average method. Finally, the weighted root mean square error is applied to evaluate the accuracy of the results. Moreover, two critical parameters, differences between positive and negative effects and the distance ratio between the accumulation area and ablation area, are discussed in detail. In the comprehensive results, the final estimated paleoglacial ELAs of the north slope of Yuju Peak and the south slope of Longquan Peak are 3,773 and 3,883 m, and their median errors are 18.73 and 45.00 m, respectively. Overall, paleoglacial ELAs in the Diancang Massif could be systematically and scientifically estimated for the first time, which is expected to provide fundamental data for accurate modeling of paleoclimatic changes in this area.
WOS关键词VALLEY GLACIERS
WOS研究方向Geology
出版者DE GRUYTER POLAND SP Z O O
WOS记录号WOS:000961086700001
源URL[http://ir.igsnrr.ac.cn/handle/311030/190458]  
专题资源与环境信息系统国家重点实验室_外文论文
作者单位1.Yunnan Univ, Sch Business & Tourism Management, Kunming, Peoples R China
2.Yunnan Univ, Sch Earth Sci, Kunming, Peoples R China
3.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, State Key Lab Resources & Environm Informat Syst, Beijing, Peoples R China
4.South China Normal Univ, Sch Comp Sci, Guangzhou, Peoples R China
推荐引用方式
GB/T 7714
Zeng, Hongyun,Li, Peng,Zhu, Yunqiang,et al. Reconstruction of paleoglacial equilibrium-line altitudes during the Last Glacial Maximum in the Diancang Massif, Northwest Yunnan Province, China[J]. OPEN GEOSCIENCES,2023,15(1):20220426.
APA Zeng, Hongyun,Li, Peng,Zhu, Yunqiang,Zhang, Jinqu,&Zhao, Xiaoqin.(2023).Reconstruction of paleoglacial equilibrium-line altitudes during the Last Glacial Maximum in the Diancang Massif, Northwest Yunnan Province, China.OPEN GEOSCIENCES,15(1),20220426.
MLA Zeng, Hongyun,et al."Reconstruction of paleoglacial equilibrium-line altitudes during the Last Glacial Maximum in the Diancang Massif, Northwest Yunnan Province, China".OPEN GEOSCIENCES 15.1(2023):20220426.

入库方式: OAI收割

来源:地理科学与资源研究所

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