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Response of snow hydrological processes to a changing climate during 1961 to 2016 in the headwater of Irtysh River Basin, Chinese Altai Mountains

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Abstract

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 δ18O values of rainfall, snowfall, meltwater, groundwater and river water for 2014–2015 hydrological year were -10.9‰, -22.3‰, -21.7‰, -15.7‰ and -16.0‰, 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.

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Acknowledgments

This study was funded by the Chinese Academy of Sciences (KJZD-EW-G03-04, QYZDJSSW- DQC039) and the National Science Foundation of China (NSFC 41630754, 41690144, 41421061). Funding was also provided by the Foundation of the State Key Laboratory of Cryospheric Sciences (SKLCS) at Northwest Institute of Eco-Environment and Resources (NIEER), CAS (SKLCS-OP-2017-10, SKLCS-ZZ- 2016). The authors are sincerely grateful to the anonymous reviewers for their suggestions and feedback, which helped improve the paper significantly.

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Authors and Affiliations

  1. State Key Laboratory of Cryospheric Sciences, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou, 730000, China

    Wei Zhang, Shi-chang Kang, Yong-ping Shen & Jian-qiao He

  2. Chinese Academy of Sciences Center for Excellence in Tibetan Plateau Earth Sciences, Beijing, 100101, China

    Shi-chang Kang

  3. University of Chinese Academy of Sciences, Beijing, 100049, China

    An-an Chen

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  1. Wei Zhang
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Correspondence to Wei Zhang.

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Zhang, W., Kang, Sc., Shen, Yp. 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. Mt. Sci. 14, 2295–2310 (2017). https://doi.org/10.1007/s11629-017-4556-z

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