中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Reversal in snow mass trends on the Tibetan Plateau and their climatic causes

文献类型:期刊论文

作者Gao, Yang1,3; Lu, Ning1,2; Dai, Yufeng3; Yao, Tandong3
刊名JOURNAL OF HYDROLOGY
出版日期2023-05-01
卷号620页码:12
ISSN号0022-1694
关键词Snow mass change Snow water equivalent Pattern transition Trend reversals Climatic causes
DOI10.1016/j.jhydrol.2023.129438
通讯作者Gao, Yang(yanggao@itpcas.ac.cn) ; Lu, Ning(lvn@lreis.ac.cn)
英文摘要The snowpack on the Tibetan Plateau (TP), which feeds ten major rivers and supplies freshwater to heavily populated downstream areas, is undergoing major changes owing to climate change. However, the impact of climate change on snowpacks is debated because of the lack of quantitative knowledge about snow mass on the TP. In this study, we collected long time-series data of the snowpack (1961-2018) from 143 stations on the TP at elevations of 1100-4800 m asl and calculated the snow water equivalent based on the observed snow depths and simulated snow densities to examine the snow mass trends, transition patterns of the trends, and their climatic causes. The results show that snow mass on the TP experienced a large increase (1.56 mm/y) until 1981 and a decrease (-0.58 mm/y) after 1981. The snow mass trends exhibited three transition patterns before and after 1981: increasing snow mass trends intensified and decreasing trends weakened on the north edge of the TP; snow loss intensified in the northeast region; and snow mass trends reversed from increasing to decreasing in the south. North of 35 degrees N, the snow mass variability was controlled by precipitation changes. South of 35 degrees N, warming affected only a few stations below 3000 m before 1981, and the reinforced warming then resulted in increased snow mass loss at almost all the stations after 1981. Warming-driven snow mass reversals and the continued warming on the TP could lead to significant water management challenges in densely populated downstream areas.
WOS关键词WATER EQUIVALENT ; VARIABILITY ; PRECIPITATION ; TEMPERATURE ; SWITZERLAND ; COVER
资助项目Natural Science Foundation of China[42171136] ; Second Tibetan Plateau Scientific Expedition and Research (STEP) program[2019QZKK0201] ; Basic Science Center for Tibetan Plateau Earth System (BSCTPES, NSFC grant) ; [41988101-03]
WOS研究方向Engineering ; Geology ; Water Resources
语种英语
出版者ELSEVIER
WOS记录号WOS:001049003300001
资助机构Natural Science Foundation of China ; Second Tibetan Plateau Scientific Expedition and Research (STEP) program ; Basic Science Center for Tibetan Plateau Earth System (BSCTPES, NSFC grant)
源URL[http://ir.igsnrr.ac.cn/handle/311030/196155]  
专题中国科学院地理科学与资源研究所
通讯作者Gao, Yang; Lu, Ning
作者单位1.16 Lincui Rd, Beijing 100101, Peoples R China
2.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, State Key Lab Resources & Environm Informat Syst, Beijing 100101, Peoples R China
3.Chinese Acad Sci, Inst Tibetan Plateau Res, State Key Lab Tibetan Plateau Earth Syst Environm, Beijing 100101, Peoples R China
推荐引用方式
GB/T 7714
Gao, Yang,Lu, Ning,Dai, Yufeng,et al. Reversal in snow mass trends on the Tibetan Plateau and their climatic causes[J]. JOURNAL OF HYDROLOGY,2023,620:12.
APA Gao, Yang,Lu, Ning,Dai, Yufeng,&Yao, Tandong.(2023).Reversal in snow mass trends on the Tibetan Plateau and their climatic causes.JOURNAL OF HYDROLOGY,620,12.
MLA Gao, Yang,et al."Reversal in snow mass trends on the Tibetan Plateau and their climatic causes".JOURNAL OF HYDROLOGY 620(2023):12.

入库方式: OAI收割

来源:地理科学与资源研究所

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