Articles | Volume 24, issue 6
https://doi.org/10.5194/hess-24-3077-2020
https://doi.org/10.5194/hess-24-3077-2020
Research article
 | 
12 Jun 2020
Research article |  | 12 Jun 2020

Future shift in winter streamflow modulated by the internal variability of climate in southern Ontario

Olivier Champagne, M. Altaf Arain, Martin Leduc, Paulin Coulibaly, and Shawn McKenzie

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: Publish subject to revisions (further review by editor and referees) (14 Nov 2019) by Chris DeBeer
AR by Olivier Champagne on behalf of the Authors (16 Dec 2019)  Author's response 
ED: Referee Nomination & Report Request started (10 Jan 2020) by Chris DeBeer
RR by Anonymous Referee #1 (11 Jan 2020)
ED: Reject (18 Feb 2020) by Chris DeBeer
ED: Publish subject to revisions (further review by editor and referees) (25 Feb 2020) by Chris DeBeer
AR by Olivier Champagne on behalf of the Authors (08 Apr 2020)  Author's response   Manuscript 
ED: Publish subject to technical corrections (12 May 2020) by Chris DeBeer
AR by Olivier Champagne on behalf of the Authors (12 May 2020)  Author's response   Manuscript 
Download
Short summary
Using 50 members of one regional climate model and a processed-based hydrological model applied in four river basins in southern Ontario, this work focused on the winter streamflow projection uncertainties for the first half of 21st century. The results show a January–February increase of streamflow for the 50 projections due to early snowmelt and a rainfall increase. The streamflow projections are also modulated by the change of pressure patterns advecting different air masses over the region.