Articles | Volume 23, issue 12
https://doi.org/10.5194/hess-23-5017-2019
https://doi.org/10.5194/hess-23-5017-2019
Research article
 | 
13 Dec 2019
Research article |  | 13 Dec 2019

Effects of preferential flow on snowmelt partitioning and groundwater recharge in frozen soils

Aaron A. Mohammed, Igor Pavlovskii, Edwin E. Cey, and Masaki Hayashi

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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 minor revisions (further review by editor) (12 Sep 2019) by Sean Carey
AR by Aaron Mohammed on behalf of the Authors (21 Oct 2019)  Author's response    Manuscript
ED: Publish as is (05 Nov 2019) by Sean Carey
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Short summary
In cold regions, the permeability of the frozen ground is an important factor influencing a watershed's response to snowmelt. This study highlights the effects of preferential flow in frozen soils on snowmelt redistribution and groundwater recharge in seasonally frozen landscapes.