Articles | Volume 24, issue 3
https://doi.org/10.5194/hess-24-1145-2020
https://doi.org/10.5194/hess-24-1145-2020
Research article
 | 
11 Mar 2020
Research article |  | 11 Mar 2020

Understanding the effects of climate warming on streamflow and active groundwater storage in an alpine catchment: the upper Lhasa River

Lu Lin, Man Gao, Jintao Liu, Jiarong Wang, Shuhong Wang, Xi Chen, and Hu Liu

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Quantifying streamflow and active groundwater storage in response to climate warming in an alpine catchment on the Tibetan Plateau
Lu Lin, Man Gao, Jintao Liu, Xi Chen, and Hu Liu
Hydrol. Earth Syst. Sci. Discuss., https://doi.org/10.5194/hess-2018-541,https://doi.org/10.5194/hess-2018-541, 2018
Manuscript not accepted for further review
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Cited articles

Bense, V. F., Kooi, H., Ferguson, G., and Read, T.: Permafrost degradation as a control on hydrogeological regime shifts in a warming climate, J. Geophys. Res.-Earth, 117, F03036, https://doi.org/10.1029/2011JF002143, 2012. 
Bibi, S., Wang, L., Li, X. P., Zhou, J., Chen, D. L., and Yao, T. D.: Climatic and associated cryospheric, biospheric, and hydrological changes on the Tibetan Plateau: A review, Int. J. Climatol., 38, e1–e17, https://doi.org/10.1002/joc.5411, 2018. 
Brutsaert, W.: Long-term groundwater storage trends estimated from streamflow records: Climatic perspective, Water Resour. Res., 44, 114–125, https://doi.org/10.1029/2007WR006518, 2008. 
Brutsaert, W. and Nieber, J. L.: Regionalized drought flow hydrographs from a mature glaciated plateau, Water Resour. Res., 13, 637–643, 1977. 
Buttle, J. M.: Mediating stream baseflow response to climate change: the role of basin storage, Hydrol. Process., 32, 363–378, https://doi.org/10.1002/hyp.11418, 2017. 
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In this paper, recession flow analysis – assuming nonlinearized outflow from aquifers into streams – was used to quantify active groundwater storage in a headwater catchment with high glacierization and large-scale frozen ground on the Tibetan Plateau. Hence, this work provides a perspective to clarify the impact of glacial retreat and frozen ground degradation due to climate change on hydrological processes.