Articles | Volume 21, issue 8
https://doi.org/10.5194/hess-21-4115-2017
https://doi.org/10.5194/hess-21-4115-2017
Research article
 | 
16 Aug 2017
Research article |  | 16 Aug 2017

Simulated hydrologic response to projected changes in precipitation and temperature in the Congo River basin

Noel Aloysius and James Saiers

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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 (23 Aug 2016) by Lixin Wang
AR by Noel Aloysius on behalf of the Authors (13 Oct 2016)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (14 Oct 2016) by Lixin Wang
RR by Anonymous Referee #3 (11 Nov 2016)
RR by Anonymous Referee #2 (19 Nov 2016)
ED: Reconsider after major revisions (further review by Editor and Referees) (26 Nov 2016) by Lixin Wang
AR by Noel Aloysius on behalf of the Authors (17 Apr 2017)
ED: Referee Nomination & Report Request started (19 Apr 2017) by Lixin Wang
RR by Anonymous Referee #3 (23 May 2017)
ED: Publish subject to minor revisions (further review by Editor) (04 Jun 2017) by Lixin Wang
AR by Noel Aloysius on behalf of the Authors (16 Jun 2017)
ED: Publish as is (25 Jun 2017) by Lixin Wang
AR by Noel Aloysius on behalf of the Authors (01 Jul 2017)  Manuscript 
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Short summary
With the aid of a hydrological model and outputs from global climate models (GCMs), we elucidate the spatiotemporal variability of rainfall–runoff in the Congo River basin in the past and in the future under multiple greenhouse gas emission scenarios. We show that the hydrologic model that is forced with outputs from 25 GCMs and two emission scenarios reveal a range of projected changes in precipitation and runoff, and that runoff dynamics are highly sensitive to GCM forcing.