中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Potential role of permafrost thaw on increasing Siberian river discharge

文献类型:期刊论文

作者Wang, Ping1,2; Huang, Qiwei1,2; Pozdniakov, Sergey P.3; Liu, Shiqi1; Ma, Ning1; Wang, Tianye4; Zhang, Yongqiang1,2; Yu, Jingjie1,2; Xie, Jiaxin1,2; Fu, Guobin5
刊名ENVIRONMENTAL RESEARCH LETTERS
出版日期2021-03-01
卷号16期号:3页码:10
ISSN号1748-9326
关键词streamflow change climate elasticity Budyko framework climate warming permafrost degradation Siberian rivers
DOI10.1088/1748-9326/abe326
通讯作者Wang, Ping(wangping@igsnrr.ac.cn)
英文摘要Despite the increasing Siberian river discharge, the sensitivity of streamflow to climate forcing/permafrost thawing is poorly quantified. Based on the Budyko framework and superposition principles, we detected and attributed the changes in streamflow regimes for the three great Siberian rivers (Ob, Yenisei, and Lena) during 1936-2019. Over the past 84 years, streamflow of Ob, Yenisei and Lena has increased by similar to 7.7%, 7.4% and 22.0%, respectively. Intensified precipitation induced by a warming climate is a major contributor to increased annual streamflow. However, winter streamflow appears to be particularly sensitive to temperature. Whilst rising temperature can reduce streamflow via evapotranspiration, it can enhance groundwater discharge to rivers due to permafrost thawing. Currently, every 1 degrees C rise in temperature likely leads to 6.1%-10.5% increase in groundwater discharge, depending on the permafrost condition. For permafrost-developed basins, the contribution to increased streamflow from thawing permafrost will continue to increase in the context of global warming.
WOS关键词WATER-BALANCE ; WINTER STREAMFLOW ; CLIMATE-CHANGE ; PRECIPITATION ; TEMPERATURE ; VARIABILITY ; BASEFLOW ; REGIME ; BASIN
资助项目NSFC-RFS[42061134017] ; NSFC-RFS[21-47-00008] ; Strategic Priority Research Program of the Chinese Academy of Sciences[XDA2003020101] ; Science and Technology Basic Resources Investigation Program of China[2017FY101302] ; Science and Technology Basic Resources Investigation Program of China[2017FY101301] ; Key Project of the Chinese Academy of Sciences[ZDRW-ZS-2017-4] ; 67th China Postdoctoral Science Foundation[2020M670434]
WOS研究方向Environmental Sciences & Ecology ; Meteorology & Atmospheric Sciences
语种英语
出版者IOP PUBLISHING LTD
WOS记录号WOS:000624490400001
资助机构NSFC-RFS ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Science and Technology Basic Resources Investigation Program of China ; Key Project of the Chinese Academy of Sciences ; 67th China Postdoctoral Science Foundation
源URL[http://ir.igsnrr.ac.cn/handle/311030/160427]  
专题中国科学院地理科学与资源研究所
通讯作者Wang, Ping
作者单位1.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Key Lab Water Cycle & Related Land Surface Proc, 11A Datun Rd, Beijing 100101, Peoples R China
2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
3.Lomonosov Moscow State Univ, Dept Hydrogeol, GSP-1, Moscow 119899, Russia
4.Zhengzhou Univ, Sch Water Conservancy Engn, 100 Sci Ave, Zhengzhou 450001, Henan, Peoples R China
5.CSIRO Land & Water, Private Bag 5, Wembley, WA 6913, Australia
6.Lomonosov Moscow State Univ, Dept Land Hydrol, GSP-1, Moscow 119991, Russia
推荐引用方式
GB/T 7714
Wang, Ping,Huang, Qiwei,Pozdniakov, Sergey P.,et al. Potential role of permafrost thaw on increasing Siberian river discharge[J]. ENVIRONMENTAL RESEARCH LETTERS,2021,16(3):10.
APA Wang, Ping.,Huang, Qiwei.,Pozdniakov, Sergey P..,Liu, Shiqi.,Ma, Ning.,...&Liu, Changming.(2021).Potential role of permafrost thaw on increasing Siberian river discharge.ENVIRONMENTAL RESEARCH LETTERS,16(3),10.
MLA Wang, Ping,et al."Potential role of permafrost thaw on increasing Siberian river discharge".ENVIRONMENTAL RESEARCH LETTERS 16.3(2021):10.

入库方式: OAI收割

来源:地理科学与资源研究所

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