Modelling the seasonal variations of soil temperatures in the Arctic coasts

The soil temperature within the Arctic coasts within the continuous permafrost is not widely measured; the temporal and spatial resolutions of the measured temperature observations are relatively high. In this study, we examined the methods to interpolate, hindcast and forecast temperature measureme...

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Published in:Polar Science
Main Authors: Islam, Mohammad Akhsanul, Lubbad, Raed, Ghoreishian Amiri, Seyed Ali, Isaev, Vladislav, Shevchuk, Yaroslav, Uvarova, Alexandra Vladimirovna, Afzal, Mohammad Saud, Kumar, Avinash
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier 2021
Subjects:
Online Access:https://hdl.handle.net/11250/2979333
https://doi.org/10.1016/j.polar.2021.100732
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spelling ftntnutrondheimi:oai:ntnuopen.ntnu.no:11250/2979333 2023-05-15T14:55:02+02:00 Modelling the seasonal variations of soil temperatures in the Arctic coasts Islam, Mohammad Akhsanul Lubbad, Raed Ghoreishian Amiri, Seyed Ali Isaev, Vladislav Shevchuk, Yaroslav Uvarova, Alexandra Vladimirovna Afzal, Mohammad Saud Kumar, Avinash 2021 application/pdf https://hdl.handle.net/11250/2979333 https://doi.org/10.1016/j.polar.2021.100732 eng eng Elsevier https://reader.elsevier.com/reader/sd/pii/S1873965221001201?token=D6779FF2D4A2A4B6F1B4D9F78B395FE1B2AD7EA7F23C8DFF7E595BCBE65AA338E7A2DF651829B51E436356873DA38546&originRegion=eu-west-1&originCreation EC/H2020/773421 Norges forskningsråd: 262644 urn:issn:1873-9652 https://hdl.handle.net/11250/2979333 https://doi.org/10.1016/j.polar.2021.100732 cristin:1960456 Attribution-NonCommercial-NoDerivatives 4.0 Internasjonal http://creativecommons.org/licenses/by-nc-nd/4.0/deed.no CC-BY-NC-ND Polar Science Peer reviewed Journal article 2021 ftntnutrondheimi https://doi.org/10.1016/j.polar.2021.100732 2022-02-23T23:38:45Z The soil temperature within the Arctic coasts within the continuous permafrost is not widely measured; the temporal and spatial resolutions of the measured temperature observations are relatively high. In this study, we examined the methods to interpolate, hindcast and forecast temperature measurements within the active layer and shallow permafrost when the temperature measurements at the surface or near the surface are available. The temperature variations along the year are periodic, and hence attempts are made to express the seasonal variations with a combination of periodic function (Fourier components); which are used as boundary conditions to reach the analytical solutions. The temperature measurements from surface to about 10 metre of depths at the Baydaratskaya Bay, Kara Sea are available. We adopted a data-driven model based on simplified analytical closed-form solution derived from the boundary conditions. The parameters of the solution are calibrated from the field measurements and validated with field observations. The model then can be used to hindcast and forecast temperature at any points within the soil. publishedVersion Article in Journal/Newspaper Arctic Baydaratskaya bay Kara Sea permafrost Polar Science Polar Science NTNU Open Archive (Norwegian University of Science and Technology) Arctic Kara Sea Polar Science 30 100732
institution Open Polar
collection NTNU Open Archive (Norwegian University of Science and Technology)
op_collection_id ftntnutrondheimi
language English
description The soil temperature within the Arctic coasts within the continuous permafrost is not widely measured; the temporal and spatial resolutions of the measured temperature observations are relatively high. In this study, we examined the methods to interpolate, hindcast and forecast temperature measurements within the active layer and shallow permafrost when the temperature measurements at the surface or near the surface are available. The temperature variations along the year are periodic, and hence attempts are made to express the seasonal variations with a combination of periodic function (Fourier components); which are used as boundary conditions to reach the analytical solutions. The temperature measurements from surface to about 10 metre of depths at the Baydaratskaya Bay, Kara Sea are available. We adopted a data-driven model based on simplified analytical closed-form solution derived from the boundary conditions. The parameters of the solution are calibrated from the field measurements and validated with field observations. The model then can be used to hindcast and forecast temperature at any points within the soil. publishedVersion
format Article in Journal/Newspaper
author Islam, Mohammad Akhsanul
Lubbad, Raed
Ghoreishian Amiri, Seyed Ali
Isaev, Vladislav
Shevchuk, Yaroslav
Uvarova, Alexandra Vladimirovna
Afzal, Mohammad Saud
Kumar, Avinash
spellingShingle Islam, Mohammad Akhsanul
Lubbad, Raed
Ghoreishian Amiri, Seyed Ali
Isaev, Vladislav
Shevchuk, Yaroslav
Uvarova, Alexandra Vladimirovna
Afzal, Mohammad Saud
Kumar, Avinash
Modelling the seasonal variations of soil temperatures in the Arctic coasts
author_facet Islam, Mohammad Akhsanul
Lubbad, Raed
Ghoreishian Amiri, Seyed Ali
Isaev, Vladislav
Shevchuk, Yaroslav
Uvarova, Alexandra Vladimirovna
Afzal, Mohammad Saud
Kumar, Avinash
author_sort Islam, Mohammad Akhsanul
title Modelling the seasonal variations of soil temperatures in the Arctic coasts
title_short Modelling the seasonal variations of soil temperatures in the Arctic coasts
title_full Modelling the seasonal variations of soil temperatures in the Arctic coasts
title_fullStr Modelling the seasonal variations of soil temperatures in the Arctic coasts
title_full_unstemmed Modelling the seasonal variations of soil temperatures in the Arctic coasts
title_sort modelling the seasonal variations of soil temperatures in the arctic coasts
publisher Elsevier
publishDate 2021
url https://hdl.handle.net/11250/2979333
https://doi.org/10.1016/j.polar.2021.100732
geographic Arctic
Kara Sea
geographic_facet Arctic
Kara Sea
genre Arctic
Baydaratskaya bay
Kara Sea
permafrost
Polar Science
Polar Science
genre_facet Arctic
Baydaratskaya bay
Kara Sea
permafrost
Polar Science
Polar Science
op_source Polar Science
op_relation https://reader.elsevier.com/reader/sd/pii/S1873965221001201?token=D6779FF2D4A2A4B6F1B4D9F78B395FE1B2AD7EA7F23C8DFF7E595BCBE65AA338E7A2DF651829B51E436356873DA38546&originRegion=eu-west-1&originCreation
EC/H2020/773421
Norges forskningsråd: 262644
urn:issn:1873-9652
https://hdl.handle.net/11250/2979333
https://doi.org/10.1016/j.polar.2021.100732
cristin:1960456
op_rights Attribution-NonCommercial-NoDerivatives 4.0 Internasjonal
http://creativecommons.org/licenses/by-nc-nd/4.0/deed.no
op_rightsnorm CC-BY-NC-ND
op_doi https://doi.org/10.1016/j.polar.2021.100732
container_title Polar Science
container_volume 30
container_start_page 100732
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