Resolving the influence of temperature forcing through heat conduction on rock glacier dynamics: a numerical  modelling approach

Cicoira, Alessandro; Beutel, Jan; Faillettaz, Jérome; Gärtner-Roer, Isabelle; Vieli, Andreas

doi:https://doi.org/10.5194/tc-13-927-2019

Articles | Volume 13, issue 3

The Cryosphere, 13, 927–942, 2019

https://doi.org/10.5194/tc-13-927-2019

© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.

The Cryosphere, 13, 927–942, 2019

https://doi.org/10.5194/tc-13-927-2019

© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 13, issue 3

Research article 18 Mar 2019

Research article | 18 Mar 2019

Resolving the influence of temperature forcing through heat conduction on rock glacier dynamics: a numerical modelling approach

Alessandro Cicoira et al.

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Final revised paper (published on 18 Mar 2019)
Preprint (discussion started on 26 Sep 2018)

Interactive discussion

Status: closed

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

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- Supplement

RC1: 'Comments to the paper by Cicoira et al.', Martin Hoelzle, 02 Dec 2018
RC2: 'Review Comments', Lukas U. Arenson, 14 Jan 2019
AC1: 'final response', Alessandro Cicoira, 18 Jan 2019

Peer-review completion

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

AR by Alessandro Cicoira on behalf of the Authors (18 Jan 2019) Author's response Manuscript

ED: Publish subject to technical corrections (13 Feb 2019) by Christian Hauck

Short summary

Rock glacier flow varies on multiple timescales. The variations have been linked to climatic forcing, but a quantitative understanding is still missing. We use a 1-D numerical modelling approach coupling heat conduction to a creep model in order to study the influence of temperature variations on rock glacier flow. Our results show that heat conduction alone cannot explain the observed variations. Other processes, likely linked to water, must dominate the short-term velocity signal.