Arid
DOI10.1016/j.jhydrol.2021.127209
The role of snowmelt discharge to runoff of an alpine watershed: Evidence from water stable isotopes
Feng, Mingming; Zhang, Wenguang; Zhang, Shaoqing; Sun, Zeyu; Li, Yang; Huang, Yiqiang; Wang, Wenjuan; Qi, Peng; Zou, Yuanchun; Jiang, Ming
通讯作者Zhang, WG ; Jiang, M (corresponding author),Chinese Acad Sci, Northeast Inst Geog & Agroecol IGA, Key Lab Wetland Ecol & Environm, Changchun 130102, Peoples R China.
来源期刊JOURNAL OF HYDROLOGY
ISSN0022-1694
EISSN1879-2707
出版年2022
卷号604
英文摘要Snow is an important form of water storage which profoundly affects the hydrological processes in alpine watersheds, especially the runoff during snowmelt period. As the strong impact of climate change, the concern about snowmelt water to runoff in alpine watersheds is dramatically growing. However, the studies are mainly focused on arid and semi-arid areas, the research on semi-humid regions sensitive to the climate change need to be strengthened. In this study, for evaluating the contribution of snowmelt water to runoff in snowmelt period, we calculated the stable isotope values (8D, 818O and d-excess) of different water bodies including river, snow, rain, groundwater, and snowmelt water in the Erdaobaihe River watershed of Changbai Mountains area. The results indicated that the 818O values of snowmelt water showed an increasing trend with increasing temperature, while the d-excess values of snowmelt water showed a decreasing trend. During the snowmelt period, the snow cover ratio varied from 20.31% to 0.02%. The contribution ratio of snowmelt water to runoff was from 14.4% to 59.8% with average of 42.60% and the total contribution discharge was about 36.56 x 106 m3, which was higher than inland mountainous areas as different elevation and climate. As the stable water source of river, the groundwater contributed 19.2-61.6% with average of 43.88%. The snowmelt water plays an important role in regional water balance. Owing to climate change, the snowfall period in Changbai Mountains was gradually shortening and extreme snowfall events were increasing. The results will provide evidence for further hydrological studies and help to plan future water management strategies in the alpine watershed.
英文关键词Snowmelt water Alpine watershed Stable isotope Changbai Mountains Climate change Semi-humid areas
类型Article
语种英语
收录类别SCI-E
WOS记录号WOS:000751952500002
WOS关键词CHANGBAI MOUNTAIN ; CLIMATE-CHANGE ; HYDROGRAPH SEPARATION ; GLACIER MELT ; COVER ; PRECIPITATION ; VARIABILITY ; DEPTH ; TREELINE ; BALANCE
WOS类目Engineering, Civil ; Geosciences, Multidisciplinary ; Water Resources
WOS研究方向Engineering ; Geology ; Water Resources
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/376898
作者单位[Feng, Mingming; Zhang, Wenguang; Zhang, Shaoqing; Sun, Zeyu; Li, Yang; Huang, Yiqiang; Wang, Wenjuan; Qi, Peng; Zou, Yuanchun; Jiang, Ming] Chinese Acad Sci, Northeast Inst Geog & Agroecol IGA, Key Lab Wetland Ecol & Environm, Changchun 130102, Peoples R China; [Feng, Mingming] Univ Chinese Acad Sci, Beijing 100049, Peoples R China; [Feng, Mingming; Zhang, Wenguang; Sun, Zeyu; Li, Yang; Huang, Yiqiang; Wang, Wenjuan; Qi, Peng; Zou, Yuanchun; Jiang, Ming] Jilin Prov Joint Key Lab Changbai Mt Wetland & Ec, Changchun 130102, Peoples R China; [Sun, Zeyu] Changchun Univ Sci & Technol, Sch Chem & Environm Engn, Changchun 130022, Peoples R China; [Li, Yang; Huang, Yiqiang] Yanbian Univ, Coll Geogragpy & Ocean Sci, Yanbian 133002, Peoples R China
推荐引用方式
GB/T 7714
Feng, Mingming,Zhang, Wenguang,Zhang, Shaoqing,et al. The role of snowmelt discharge to runoff of an alpine watershed: Evidence from water stable isotopes[J],2022,604.
APA Feng, Mingming.,Zhang, Wenguang.,Zhang, Shaoqing.,Sun, Zeyu.,Li, Yang.,...&Jiang, Ming.(2022).The role of snowmelt discharge to runoff of an alpine watershed: Evidence from water stable isotopes.JOURNAL OF HYDROLOGY,604.
MLA Feng, Mingming,et al."The role of snowmelt discharge to runoff of an alpine watershed: Evidence from water stable isotopes".JOURNAL OF HYDROLOGY 604(2022).
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