Articles | Volume 9, issue 5
https://doi.org/10.5194/tc-9-1857-2015
https://doi.org/10.5194/tc-9-1857-2015
Research article
 | 
23 Sep 2015
Research article |  | 23 Sep 2015

A macroscale mixture theory analysis of deposition and sublimation rates during heat and mass transfer in dry snow

A. C. Hansen and W. E. Foslien

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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
AR by Andrew Hansen on behalf of the Authors (15 May 2015)  Author's response 
ED: Referee Nomination & Report Request started (31 May 2015) by Martin Schneebeli
RR by Anonymous Referee #2 (15 Jun 2015)
RR by Henning Löwe (16 Jun 2015)
ED: Reconsider after major revisions (17 Jun 2015) by Martin Schneebeli
AR by Andrew Hansen on behalf of the Authors (22 Jun 2015)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (01 Jul 2015) by Martin Schneebeli
RR by Anonymous Referee #2 (20 Jul 2015)
RR by Henning Löwe (27 Jul 2015)
ED: Publish subject to minor revisions (Editor review) (07 Aug 2015) by Martin Schneebeli
AR by Andrew Hansen on behalf of the Authors (11 Aug 2015)  Author's response   Manuscript 
ED: Publish subject to technical corrections (21 Aug 2015) by Martin Schneebeli
AR by Andrew Hansen on behalf of the Authors (23 Aug 2015)  Author's response   Manuscript 
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Short summary
We implement a continuum mixture theory to elucidate coupled heat and mass transfer phenomena occurring in a snow cover. The effects of mass transfer near the ground, near the surface including diurnal temperature effects, as well as adjacent to an ice crust are examined. The analysis requires an accurate assessment of thermal conductivity and the mass diffusion coefficient for snow. An analytical model for these parameters is developed, showing remarkable agreement with numerical models.