Articles | Volume 21, issue 9
Hydrol. Earth Syst. Sci., 21, 4803–4823, 2017
https://doi.org/10.5194/hess-21-4803-2017
Hydrol. Earth Syst. Sci., 21, 4803–4823, 2017
https://doi.org/10.5194/hess-21-4803-2017

Research article 27 Sep 2017

Research article | 27 Sep 2017

Hydrological connectivity from glaciers to rivers in the Qinghai–Tibet Plateau: roles of suprapermafrost and subpermafrost groundwater

Rui Ma et al.

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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) (25 Apr 2017) by Bill X. Hu
AR by Anna Wenzel on behalf of the Authors (30 May 2017)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (23 Jun 2017) by Bill X. Hu
RR by Anonymous Referee #1 (24 Jun 2017)
RR by Anonymous Referee #3 (19 Jul 2017)
ED: Publish subject to technical corrections (07 Aug 2017) by Bill X. Hu
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Short summary
The roles of groundwater flow in the hydrological cycle within the alpine area characterized by permafrost or seasonal frost are poorly known. We investigated the role of permafrost in controlling groundwater flow and hydrological connections between glaciers and river. The recharge, flow path and discharge of permafrost groundwater at the study site were explored. Two mechanisms were proposed to explain the significantly seasonal variation in interaction between groundwater and surface water.