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...
Main Authors: | , , |
---|---|
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
International Journal of Open Information Technologies
2023
|
Subjects: | |
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 |