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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Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish subject to revisions (further review by editor and referees) (12 Sep 2019) by Fuqiang Tian
AR by Jintao Liu on behalf of the Authors (24 Sep 2019)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (25 Sep 2019) by Fuqiang Tian
RR by Anonymous Referee #2 (14 Oct 2019)
RR by Anonymous Referee #1 (26 Oct 2019)
ED: Publish subject to revisions (further review by editor and referees) (08 Nov 2019) by Fuqiang Tian
AR by Jintao Liu on behalf of the Authors (28 Nov 2019)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (18 Dec 2019) by Fuqiang Tian
RR by Anonymous Referee #2 (23 Dec 2019)
RR by Anonymous Referee #1 (31 Jan 2020)
ED: Publish as is (31 Jan 2020) by Fuqiang Tian
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Short summary
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.