Dynamics of the temperature regime of permafrost soil and ice thickness during climate change

The study of the initial-boundary value problem for a non-stationary one-dimensional heat conduction equation, which models the temperature distribution of permafrost soil and ice thickness, was carried out. A mathematical model is constructed taking into account solid-liquid phase transitions. To d...

Full description

Bibliographic Details
Main Authors: Fedotov, Anatoly, Kaniber, Vladimir, Khrapov, Pavel
Format: Article in Journal/Newspaper
Language:English
Published: International Journal of Open Information Technologies 2023
Subjects:
Ice
Online Access:http://injoit.org/index.php/j1/article/view/1516
id ftjinjoit:oai:ojs.injoit.org:article/1516
record_format openpolar
spelling ftjinjoit:oai:ojs.injoit.org:article/1516 2023-06-11T04:12:33+02:00 Dynamics of the temperature regime of permafrost soil and ice thickness during climate change Fedotov, Anatoly Kaniber, Vladimir Khrapov, Pavel 2023-05-01 application/pdf http://injoit.org/index.php/j1/article/view/1516 eng eng International Journal of Open Information Technologies http://injoit.org/index.php/j1/article/view/1516/1442 http://injoit.org/index.php/j1/article/view/1516 Copyright (c) 2023 International Journal of Open Information Technologies International Journal of Open Information Technologies; Vol 11, No 5 (2023); 106-113 2307-8162 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2023 ftjinjoit 2023-05-02T17:00:18Z The study of the initial-boundary value problem for a non-stationary one-dimensional heat conduction equation, which models the temperature distribution of permafrost soil and ice thickness, was carried out. A mathematical model is constructed taking into account solid-liquid phase transitions. To determine the parameters of the model, data from a meteorological station and reports on engineering and geological surveys were used, with the help of which the necessary physical and thermal characteristics of the computational area were obtained. The finite volume method was used to solve the problem numerically. For a steady-state periodic regime, dependences of average monthly temperatures on depth for each month are constructed, the depth of seasonal thawing and freezing, as well as the depth of zero amplitudes are found. The forecast of the temperature regime for 2100 is modeled according to the selected scenarios of the Representative Concentration Pathway (RCP) of global warming. The scenarios are based on the IPCC AR5 and SP databases, as well as taking into account the existing policy framework and the stated policy intentions of the IEA Stated Policies Scenario (STEPS). The modeling performed clearly confirmed the impact of global warming on the cryosphere of our planet. Article in Journal/Newspaper Ice permafrost International Journal of Open Information Technologies (INJOIT)
institution Open Polar
collection International Journal of Open Information Technologies (INJOIT)
op_collection_id ftjinjoit
language English
description The study of the initial-boundary value problem for a non-stationary one-dimensional heat conduction equation, which models the temperature distribution of permafrost soil and ice thickness, was carried out. A mathematical model is constructed taking into account solid-liquid phase transitions. To determine the parameters of the model, data from a meteorological station and reports on engineering and geological surveys were used, with the help of which the necessary physical and thermal characteristics of the computational area were obtained. The finite volume method was used to solve the problem numerically. For a steady-state periodic regime, dependences of average monthly temperatures on depth for each month are constructed, the depth of seasonal thawing and freezing, as well as the depth of zero amplitudes are found. The forecast of the temperature regime for 2100 is modeled according to the selected scenarios of the Representative Concentration Pathway (RCP) of global warming. The scenarios are based on the IPCC AR5 and SP databases, as well as taking into account the existing policy framework and the stated policy intentions of the IEA Stated Policies Scenario (STEPS). The modeling performed clearly confirmed the impact of global warming on the cryosphere of our planet.
format Article in Journal/Newspaper
author Fedotov, Anatoly
Kaniber, Vladimir
Khrapov, Pavel
spellingShingle Fedotov, Anatoly
Kaniber, Vladimir
Khrapov, Pavel
Dynamics of the temperature regime of permafrost soil and ice thickness during climate change
author_facet Fedotov, Anatoly
Kaniber, Vladimir
Khrapov, Pavel
author_sort Fedotov, Anatoly
title Dynamics of the temperature regime of permafrost soil and ice thickness during climate change
title_short Dynamics of the temperature regime of permafrost soil and ice thickness during climate change
title_full Dynamics of the temperature regime of permafrost soil and ice thickness during climate change
title_fullStr Dynamics of the temperature regime of permafrost soil and ice thickness during climate change
title_full_unstemmed Dynamics of the temperature regime of permafrost soil and ice thickness during climate change
title_sort dynamics of the temperature regime of permafrost soil and ice thickness during climate change
publisher International Journal of Open Information Technologies
publishDate 2023
url http://injoit.org/index.php/j1/article/view/1516
genre Ice
permafrost
genre_facet Ice
permafrost
op_source International Journal of Open Information Technologies; Vol 11, No 5 (2023); 106-113
2307-8162
op_relation http://injoit.org/index.php/j1/article/view/1516/1442
http://injoit.org/index.php/j1/article/view/1516
op_rights Copyright (c) 2023 International Journal of Open Information Technologies
_version_ 1768388500034420736