Preprints
https://doi.org/10.5194/egusphere-2024-2575
https://doi.org/10.5194/egusphere-2024-2575
02 Sep 2024
 | 02 Sep 2024

Improved permafrost modeling in mountain environments by including air convection in a hydrological model

Gerardo Zegers, Masaki Hayashi, and Rodrigo Pérez-Illanes

Abstract. Permafrost occurrence in mountainous regions is influenced by complex topography and surficial geology, leading to high spatial heterogeneity. Coarse sediments create a unique thermal regime that allows permafrost to persist even under positive mean annual air temperatures due to natural convection lowering ground temperatures. Although this process has been recognized as a key factor in explaining the persistence of permafrost formation within coarse sediments, studies assessing the impact of natural convection on ground temperatures and permafrost are limited, partly due to the absence of hydrological models that take this process into account. This article expands on a well-established hydrological model to incorporate the effects of natural air convection on heat transfer. The modified model includes airflow through Darcy’s equation and the Oberbeck-Boussinesq approximation to account for density-driven buoyancy effects, as well as a heat advection-conduction equation for the air phase without assuming local thermal equilibrium between the air and the other phases. The model was tested on a talus slope in the Canadian Rockies, where conventional models failed to represent field-based evidence of permafrost. The results revealed that coarse-size sediments can lower ground temperatures by several degrees when natural convection is considered. Additionally, the study demonstrated that the local thermal equilibrium approach hinders the impact of natural convection. This enhanced model improves our understanding of permafrost dynamics in alpine landforms and enables a more accurate analysis of permafrost extent and its influence on groundwater discharges.

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Journal article(s) based on this preprint

29 Sep 2025
Improved permafrost modelling in mountain environments by including air convection in a hydrological model
Gerardo Zegers, Masaki Hayashi, and Rodrigo Pérez-Illanes
The Cryosphere, 19, 4091–4112, https://doi.org/10.5194/tc-19-4091-2025,https://doi.org/10.5194/tc-19-4091-2025, 2025
Short summary
Gerardo Zegers, Masaki Hayashi, and Rodrigo Pérez-Illanes

Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • CC1: 'Comment on egusphere-2024-2575', Giacomo Medici, 06 Sep 2024
  • RC1: 'Comment on egusphere-2024-2575', Anonymous Referee #1, 11 Nov 2024
  • RC2: 'Comment on egusphere-2024-2575', Martin Hoelzle & Dominik Amschwand (co-review team), 17 Feb 2025

Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • CC1: 'Comment on egusphere-2024-2575', Giacomo Medici, 06 Sep 2024
  • RC1: 'Comment on egusphere-2024-2575', Anonymous Referee #1, 11 Nov 2024
  • RC2: 'Comment on egusphere-2024-2575', Martin Hoelzle & Dominik Amschwand (co-review team), 17 Feb 2025

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Publish subject to minor revisions (review by editor) (28 Apr 2025) by Adrian Flores Orozco
AR by Gerardo Zegers on behalf of the Authors (22 May 2025)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (03 Jun 2025) by Adrian Flores Orozco
AR by Gerardo Zegers on behalf of the Authors (10 Jun 2025)  Author's response   Manuscript 

Journal article(s) based on this preprint

29 Sep 2025
Improved permafrost modelling in mountain environments by including air convection in a hydrological model
Gerardo Zegers, Masaki Hayashi, and Rodrigo Pérez-Illanes
The Cryosphere, 19, 4091–4112, https://doi.org/10.5194/tc-19-4091-2025,https://doi.org/10.5194/tc-19-4091-2025, 2025
Short summary
Gerardo Zegers, Masaki Hayashi, and Rodrigo Pérez-Illanes

Model code and software

GeoTOP-CE Gerardo Zegers https://github.com/gzegers/geotop-CE

Gerardo Zegers, Masaki Hayashi, and Rodrigo Pérez-Illanes

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Latest update: 29 Sep 2025
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Short summary
This research showed that airflow within sediment accumulations promotes cooling and sustains mountain permafrost. By enhancing a numerical model, we showed that natural air movement, driven by temperature differences between sediments and external air, allows permafrost to survive. Our work aids in predicting where and how permafrost exists, which is essential for understanding its role in mountain water systems and its response to climate change.
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