Articles | Volume 19, issue 11
Hydrol. Earth Syst. Sci., 19, 4689–4705, 2015
https://doi.org/10.5194/hess-19-4689-2015
Hydrol. Earth Syst. Sci., 19, 4689–4705, 2015
https://doi.org/10.5194/hess-19-4689-2015

Research article 27 Nov 2015

Research article | 27 Nov 2015

Defining high-flow seasons using temporal streamflow patterns from a global model

D. Lee et al.

Download

Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (28 Jul 2015) by Ross Woods
AR by Donghoon Lee on behalf of the Authors (03 Aug 2015)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (04 Aug 2015) by Ross Woods
RR by Anonymous Referee #1 (04 Aug 2015)
RR by Anonymous Referee #2 (18 Aug 2015)
ED: Reconsider after major revisions (27 Aug 2015) by Ross Woods
AR by Donghoon Lee on behalf of the Authors (01 Oct 2015)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (15 Oct 2015) by Ross Woods
RR by Anonymous Referee #2 (29 Oct 2015)
ED: Publish subject to minor revisions (Editor review) (29 Oct 2015) by Ross Woods
AR by Donghoon Lee on behalf of the Authors (06 Nov 2015)  Author's response    Manuscript
ED: Publish as is (09 Nov 2015) by Ross Woods
Download
Short summary
This paper presents a global approach to defining high-flow seasons by identifying temporal patterns of streamflow. Simulations of streamflow from the PCR-GLOBWB model are evaluated to define dominant and minor high-flow seasons globally, and verified with GRDC observations and flood records from Dartmouth Flood Observatory.