Articles | Volume 21, issue 7
https://doi.org/10.5194/hess-21-3483-2017
https://doi.org/10.5194/hess-21-3483-2017
Research article
 | 
12 Jul 2017
Research article |  | 12 Jul 2017

Simulating cold-region hydrology in an intensively drained agricultural watershed in Manitoba, Canada, using the Cold Regions Hydrological Model

Marcos R. C. Cordeiro, Henry F. Wilson, Jason Vanrobaeys, John W. Pomeroy, Xing Fang, and The Red-Assiniboine Project Biophysical Modelling Team

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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: Publish subject to revisions (further review by Editor and Referees) (14 Feb 2017) by Fuqiang Tian
AR by Marcos Cordeiro on behalf of the Authors (28 Mar 2017)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (10 Apr 2017) by Fuqiang Tian
RR by Anonymous Referee #1 (19 Apr 2017)
RR by Anonymous Referee #2 (13 May 2017)
ED: Publish subject to minor revisions (further review by Editor) (13 May 2017) by Fuqiang Tian
AR by Marcos Cordeiro on behalf of the Authors (23 May 2017)  Author's response   Manuscript 
ED: Publish as is (31 May 2017) by Fuqiang Tian
AR by Marcos Cordeiro on behalf of the Authors (08 Jun 2017)
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Short summary
The physically based Cold Regions Hydrological Model (CRHM) was utilized to simulate runoff in the La Salle River, located in the northern Great Plains with flat topography, clay soils, and surface drainage. Snow sublimation and transport as well as infiltration to frozen soils were identified as critical in defining snowmelt. Challenges in representing infiltration into frozen but dry clay soils and flow routing under both dry and flooded conditions indicate the need for further study.