Initialization of thermal models in cold and warm permafrost

Equilibrium modelling, also known as spin-up, is a technique for initializing a stable thermal regime in ground temperature models for permafrost regions. The results act as a baseline for subsequent transient analyses of ground temperature response to climate change or infrastructure. In practice,...

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Published in:Arctic Science
Main Authors: Cameron Ross, Greg Siemens, Ryley Beddoe
Format: Article in Journal/Newspaper
Language:English
French
Published: Canadian Science Publishing 2022
Subjects:
Online Access:https://doi.org/10.1139/as-2021-0013
https://doaj.org/article/d561efc253b04ee5a2d2a4f54cb98d6c
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spelling ftdoajarticles:oai:doaj.org/article:d561efc253b04ee5a2d2a4f54cb98d6c 2023-05-15T14:23:47+02:00 Initialization of thermal models in cold and warm permafrost Cameron Ross Greg Siemens Ryley Beddoe 2022-06-01T00:00:00Z https://doi.org/10.1139/as-2021-0013 https://doaj.org/article/d561efc253b04ee5a2d2a4f54cb98d6c EN FR eng fre Canadian Science Publishing https://cdnsciencepub.com/doi/10.1139/as-2021-0013 https://doaj.org/toc/2368-7460 doi:10.1139/as-2021-0013 2368-7460 https://doaj.org/article/d561efc253b04ee5a2d2a4f54cb98d6c Arctic Science, Vol 8, Iss 2, Pp 362-394 (2022) permafrost model spin-up equilibrium modelling surface energy balance thermal modelling modèle de pergélisol Environmental sciences GE1-350 Environmental engineering TA170-171 article 2022 ftdoajarticles https://doi.org/10.1139/as-2021-0013 2022-12-30T22:56:48Z Equilibrium modelling, also known as spin-up, is a technique for initializing a stable thermal regime in ground temperature models for permafrost regions. The results act as a baseline for subsequent transient analyses of ground temperature response to climate change or infrastructure. In practice, spin-up procedures are often loosely described or neglected, and the criteria by which a stable thermal regime is evaluated are rarely defined or presented explicitly. In this paper, model results show that no single criterion based on thresholds of inter-cycle temperature change can be used to identify a stable thermal regime in all spin-up scenarios. Results from simulations using a wide range of initialization temperatures and conditions show the number of spin-up cycles can range between 10 and 10 000, and a spin-up criterion as fine as 0.00001 °C/cycle is required to achieve a stable thermal regime suitable for deeper warm permafrost models. The implications of selected threshold criteria are examined in follow-up transient analyses and show that warm permafrost models can be highly sensitive to initial temperature profiles based on the criterion used. The results alert scientists and engineers to the importance of initialization on site-specific and regional permafrost models for transient ground temperature analyses. Article in Journal/Newspaper Arctic permafrost pergélisol Directory of Open Access Journals: DOAJ Articles Arctic Science 8 2 362 394
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
French
topic permafrost model
spin-up
equilibrium modelling
surface energy balance
thermal modelling
modèle de pergélisol
Environmental sciences
GE1-350
Environmental engineering
TA170-171
spellingShingle permafrost model
spin-up
equilibrium modelling
surface energy balance
thermal modelling
modèle de pergélisol
Environmental sciences
GE1-350
Environmental engineering
TA170-171
Cameron Ross
Greg Siemens
Ryley Beddoe
Initialization of thermal models in cold and warm permafrost
topic_facet permafrost model
spin-up
equilibrium modelling
surface energy balance
thermal modelling
modèle de pergélisol
Environmental sciences
GE1-350
Environmental engineering
TA170-171
description Equilibrium modelling, also known as spin-up, is a technique for initializing a stable thermal regime in ground temperature models for permafrost regions. The results act as a baseline for subsequent transient analyses of ground temperature response to climate change or infrastructure. In practice, spin-up procedures are often loosely described or neglected, and the criteria by which a stable thermal regime is evaluated are rarely defined or presented explicitly. In this paper, model results show that no single criterion based on thresholds of inter-cycle temperature change can be used to identify a stable thermal regime in all spin-up scenarios. Results from simulations using a wide range of initialization temperatures and conditions show the number of spin-up cycles can range between 10 and 10 000, and a spin-up criterion as fine as 0.00001 °C/cycle is required to achieve a stable thermal regime suitable for deeper warm permafrost models. The implications of selected threshold criteria are examined in follow-up transient analyses and show that warm permafrost models can be highly sensitive to initial temperature profiles based on the criterion used. The results alert scientists and engineers to the importance of initialization on site-specific and regional permafrost models for transient ground temperature analyses.
format Article in Journal/Newspaper
author Cameron Ross
Greg Siemens
Ryley Beddoe
author_facet Cameron Ross
Greg Siemens
Ryley Beddoe
author_sort Cameron Ross
title Initialization of thermal models in cold and warm permafrost
title_short Initialization of thermal models in cold and warm permafrost
title_full Initialization of thermal models in cold and warm permafrost
title_fullStr Initialization of thermal models in cold and warm permafrost
title_full_unstemmed Initialization of thermal models in cold and warm permafrost
title_sort initialization of thermal models in cold and warm permafrost
publisher Canadian Science Publishing
publishDate 2022
url https://doi.org/10.1139/as-2021-0013
https://doaj.org/article/d561efc253b04ee5a2d2a4f54cb98d6c
genre Arctic
permafrost
pergélisol
genre_facet Arctic
permafrost
pergélisol
op_source Arctic Science, Vol 8, Iss 2, Pp 362-394 (2022)
op_relation https://cdnsciencepub.com/doi/10.1139/as-2021-0013
https://doaj.org/toc/2368-7460
doi:10.1139/as-2021-0013
2368-7460
https://doaj.org/article/d561efc253b04ee5a2d2a4f54cb98d6c
op_doi https://doi.org/10.1139/as-2021-0013
container_title Arctic Science
container_volume 8
container_issue 2
container_start_page 362
op_container_end_page 394
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