Articles | Volume 23, issue 2
https://doi.org/10.5194/hess-23-741-2019
https://doi.org/10.5194/hess-23-741-2019
Research article
 | 
08 Feb 2019
Research article |  | 08 Feb 2019

Parameter-state ensemble thinning for short-term hydrological prediction

Bruce Davison, Vincent Fortin, Alain Pietroniro, Man K. Yau, and Robert Leconte

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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) (18 Feb 2018) by Harrie-Jan Hendricks Franssen
AR by Bruce Davison on behalf of the Authors (30 Apr 2018)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (02 May 2018) by Harrie-Jan Hendricks Franssen
RR by Anonymous Referee #2 (07 Jun 2018)
RR by Anonymous Referee #1 (13 Jun 2018)
RR by Jasper Vrugt (02 Jul 2018)
ED: Reconsider after major revisions (further review by editor and referees) (08 Jul 2018) by Harrie-Jan Hendricks Franssen
AR by Bruce Davison on behalf of the Authors (13 Aug 2018)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (16 Aug 2018) by Harrie-Jan Hendricks Franssen
RR by Anonymous Referee #1 (21 Sep 2018)
RR by Jasper Vrugt (25 Oct 2018)
ED: Publish subject to revisions (further review by editor and referees) (25 Oct 2018) by Harrie-Jan Hendricks Franssen
AR by Bruce Davison on behalf of the Authors (04 Dec 2018)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (09 Dec 2018) by Harrie-Jan Hendricks Franssen
RR by Jasper Vrugt (09 Dec 2018)
ED: Publish as is (10 Dec 2018) by Harrie-Jan Hendricks Franssen
AR by Bruce Davison on behalf of the Authors (18 Dec 2018)
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Short summary
This paper explores a new method of predicting streamflow using a complex model. It makes use of streamflow observations to reduce an existing ensemble of model runs for predictive purposes. The study illustrated that the method could work given the proper constraints, which were only possible if there was enough knowledge about how the river responded to precipitation in the previous months. Ideas were discussed to allow the method to be used in a way to predict future streamflow.