On the appropriate definition of soil profile configuration and initial conditions for land surface–hydrology models  in cold regions

Sapriza-Azuri, Gonzalo; Gamazo, Pablo; Razavi, Saman; Wheater, Howard S.

doi:https://doi.org/10.5194/hess-22-3295-2018

Articles | Volume 22, issue 6

https://doi.org/10.5194/hess-22-3295-2018

© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Special issue:

Understanding and predicting Earth system and hydrological...

https://doi.org/10.5194/hess-22-3295-2018

© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 22, issue 6

Research article

|

13 Jun 2018

Research article |

| 13 Jun 2018

On the appropriate definition of soil profile configuration and initial conditions for land surface–hydrology models in cold regions

Gonzalo Sapriza-Azuri, Pablo Gamazo, Saman Razavi, and Howard S. Wheater

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Final revised paper (published on 13 Jun 2018)
Preprint (discussion started on 27 Oct 2017)

Interactive discussion

Status: closed

AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment

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- Supplement

RC1: 'Review of hess-2017-614', Anonymous Referee #1, 26 Dec 2017
- AC1: 'Response to Referee 1', Gonzalo Sapriza-Azuri, 11 Feb 2018
RC2: 'Review of Sapriza-Azuri et al.', Anonymous Referee #2, 16 Jan 2018
- AC2: 'Response to Anonymous Referee #2', Gonzalo Sapriza-Azuri, 12 Feb 2018

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision

ED: Publish subject to revisions (further review by editor and referees) (27 Feb 2018) by Sean Carey

AR by Gonzalo Sapriza-Azuri on behalf of the Authors (06 Apr 2018) Author's response Manuscript

ED: Referee Nomination & Report Request started (23 Apr 2018) by Sean Carey

RR by Anonymous Referee #2 (30 May 2018)

ED: Publish as is (30 May 2018) by Sean Carey

Short summary

Arctic and subarctic regions are amongst the most susceptible regions on Earth to climate change. There, models require a proper representation of the interactions between climate and hydrology. Typically these model represent the soil with shallow depths, whereas for cold regions, deep soil is needed. To address this, we run model experiments to characterize the effect of soil depth and temperature soil initialization. Our results demonstrate that 20 m of soil profile is essential.