Articles | Volume 24, issue 11
Hydrol. Earth Syst. Sci., 24, 5423–5438, 2020
https://doi.org/10.5194/hess-24-5423-2020
Hydrol. Earth Syst. Sci., 24, 5423–5438, 2020
https://doi.org/10.5194/hess-24-5423-2020

Research article 19 Nov 2020

Research article | 19 Nov 2020

Effects of climate anomalies on warm-season low flows in Switzerland

Marius G. Floriancic et al.

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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: Reconsider after major revisions (further review by editor and referees) (26 Nov 2019) by Kerstin Stahl
AR by Marius Floriancic on behalf of the Authors (21 Apr 2020)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (27 Apr 2020) by Kerstin Stahl
RR by Anonymous Referee #3 (20 May 2020)
RR by Anonymous Referee #2 (21 May 2020)
ED: Reconsider after major revisions (further review by editor and referees) (09 Jun 2020) by Kerstin Stahl
AR by Marius Floriancic on behalf of the Authors (05 Aug 2020)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (28 Aug 2020) by Kerstin Stahl
RR by Anonymous Referee #2 (21 Sep 2020)
ED: Publish subject to technical corrections (04 Oct 2020) by Kerstin Stahl
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Short summary
Low river flows affect societies and ecosystems. Here we study how precipitation and potential evapotranspiration shape low flows across a network of 380 Swiss catchments. Low flows in these rivers typically result from below-average precipitation and above-average potential evapotranspiration. Extreme low flows result from long periods of the combined effects of both drivers.