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DOI10.1007/s11629-017-4556-z
Response of snow hydrological processes to a changing climate during 1961 to 2016 in the headwater of Irtysh River Basin, Chinese Altai Mountains
Zhang Wei1; Kang Shi-chang1,2; Shen Yong-ping1; He Jian-qiao1; Chen An-an1,3
发表日期2017
ISSN1672-6316
EISSN1993-0321
卷号14期号:11页码:2295-2310
英文摘要

With changing climatic conditions and snow cover regime, regional hydrological cycle for a snowy basin will change and further available surface water resources will be redistributed. Assessing snow meltwater effect on runoff is the key to water safety, under climate warming and fast social-economic developing status. In this study, stable isotopic technology was utilized to analyze the snow meltwater effect on regional hydrological processes, and to declare the response of snow hydrology to climate change and snow cover regime, together with longterm meteorological and hydrological observations, in the headwater of Irtysh River, Chinese Altai Mountains during 1961-2015. The average delta 18O values of rainfall, snowfall, meltwater, groundwater and river water for 2014-2015 hydrological year were -10.9aEuro degrees, -22.3aEuro degrees, -21.7aEuro degrees, -15.7aEuro degrees and -16.0aEuro degrees, respectively. The results from stable isotopes, snow melting observation and remote sensing indicated that the meltwater effect on hydrological processes in Kayiertesi River Basin mainly occurred during snowmelt supplying period from April to June. The contribution of meltwater to runoff reached 58.1% during this period, but rainfall, meltwater and groundwater supplied 49.1%, 36.9% and 14.0% of water resource to annual runoff, respectively. With rising air temperature and increasing snowfall in cold season, the snow water equivalent (SWE) had an increasing trend but the snow cover duration declined by about one month including 13-day delay of the first day and 17-day advancement of the end day during 1961-2016. Increase in SWE provided more available water resource. However, variations in snow cover timing had resulted in redistribution of surface water resource, represented by an increase of discharge percentage in April and May, and a decline in June and July. This trend of snow hydrology will render a deficit of water resource in June and July when the water resource demand is high for agricultural irrigation and industrial manufacture.


英文关键词Irtysh River Basin;Chinese Altai Mountains;Snow hydrology;Isotope;Climate change
语种英语
WOS研究方向Environmental Sciences & Ecology
来源期刊JOURNAL OF MOUNTAIN SCIENCE
来源机构中国科学院西北资源环境生态研究院
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/89650
作者单位1.Chinese Acad Sci, Northwest Inst Ecoenvironm & Resources, State Key Lab Cryospher Sci, Lanzhou 730000, Gansu, Peoples R China;;
2.Chinese Acad Sci, Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China;;
3.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
推荐引用方式
GB/T 7714
Zhang Wei,Kang Shi-chang,Shen Yong-ping,et al. Response of snow hydrological processes to a changing climate during 1961 to 2016 in the headwater of Irtysh River Basin, Chinese Altai Mountains[J]. 中国科学院西北资源环境生态研究院,2017,14(11):2295-2310.
APA Zhang Wei,Kang Shi-chang,Shen Yong-ping,He Jian-qiao,&Chen An-an.(2017).Response of snow hydrological processes to a changing climate during 1961 to 2016 in the headwater of Irtysh River Basin, Chinese Altai Mountains.JOURNAL OF MOUNTAIN SCIENCE,14(11),2295-2310.
MLA Zhang Wei,et al."Response of snow hydrological processes to a changing climate during 1961 to 2016 in the headwater of Irtysh River Basin, Chinese Altai Mountains".JOURNAL OF MOUNTAIN SCIENCE 14.11(2017):2295-2310.
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