Articles | Volume 20, issue 1
https://doi.org/10.5194/hess-20-257-2016
https://doi.org/10.5194/hess-20-257-2016
Research article
 | 
18 Jan 2016
Research article |  | 18 Jan 2016

Time series of tritium, stable isotopes and chloride reveal short-term variations in groundwater contribution to a stream

C. Duvert, M. K. Stewart, D. I. Cendón, and M. Raiber

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AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish subject to minor revisions (Editor review) (29 Oct 2015) by Laurent Pfister
AR by Clément Duvert on behalf of the Authors (09 Nov 2015)  Author's response   Manuscript 
ED: Publish subject to technical corrections (11 Dec 2015) by Laurent Pfister
AR by Clément Duvert on behalf of the Authors (16 Dec 2015)  Manuscript 
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Short summary
The transit time of water is a key indicator of hydrological processes at the catchment scale. Our results suggest that the use of tritium time series in streamwater can be highly valuable for assessing the temporal variations in the transit time of older groundwater contributions to streamflow. We also show that, shortly after high flow events, the transit time of the old water fraction increases and tends to approach the groundwater residence time.