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,...

Full description

Bibliographic Details
Published in:Arctic Science
Main Authors: Ross, Cameron, Siemens, Greg, Beddoe, Ryley
Other Authors: LafreniȲre, Melissa
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 2022
Subjects:
Online Access:http://dx.doi.org/10.1139/as-2021-0013
https://cdnsciencepub.com/doi/full-xml/10.1139/as-2021-0013
https://cdnsciencepub.com/doi/pdf/10.1139/as-2021-0013
id crcansciencepubl:10.1139/as-2021-0013
record_format openpolar
spelling crcansciencepubl:10.1139/as-2021-0013 2024-09-15T17:49:58+00:00 Initialization of thermal models in cold and warm permafrost Ross, Cameron Siemens, Greg Beddoe, Ryley LafreniȲre, Melissa 2022 http://dx.doi.org/10.1139/as-2021-0013 https://cdnsciencepub.com/doi/full-xml/10.1139/as-2021-0013 https://cdnsciencepub.com/doi/pdf/10.1139/as-2021-0013 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Arctic Science volume 8, issue 2, page 362-394 ISSN 2368-7460 2368-7460 journal-article 2022 crcansciencepubl https://doi.org/10.1139/as-2021-0013 2024-08-01T04:10:01Z 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 Canadian Science Publishing Arctic Science 1 33
institution Open Polar
collection Canadian Science Publishing
op_collection_id crcansciencepubl
language English
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.
author2 LafreniȲre, Melissa
format Article in Journal/Newspaper
author Ross, Cameron
Siemens, Greg
Beddoe, Ryley
spellingShingle Ross, Cameron
Siemens, Greg
Beddoe, Ryley
Initialization of thermal models in cold and warm permafrost
author_facet Ross, Cameron
Siemens, Greg
Beddoe, Ryley
author_sort Ross, Cameron
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 http://dx.doi.org/10.1139/as-2021-0013
https://cdnsciencepub.com/doi/full-xml/10.1139/as-2021-0013
https://cdnsciencepub.com/doi/pdf/10.1139/as-2021-0013
genre Arctic
permafrost
genre_facet Arctic
permafrost
op_source Arctic Science
volume 8, issue 2, page 362-394
ISSN 2368-7460 2368-7460
op_rights http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining
op_doi https://doi.org/10.1139/as-2021-0013
container_title Arctic Science
container_start_page 1
op_container_end_page 33
_version_ 1810291811263971328