Modelling the seasonal variations of soil temperatures in the Arctic coasts

Abstract 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...

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Published in:Polar Science
Main Authors: Islam, Mohammad Akhsanul, Lubbad, Raed
Format: Article in Journal/Newspaper
Language:unknown
Published: Zenodo 2021
Subjects:
Online Access:https://doi.org/10.1016/j.polar.2021.100732
id ftzenodo:oai:zenodo.org:5221400
record_format openpolar
spelling ftzenodo:oai:zenodo.org:5221400 2024-09-15T17:58:17+00:00 Modelling the seasonal variations of soil temperatures in the Arctic coasts Islam, Mohammad Akhsanul Lubbad, Raed 2021-08-11 https://doi.org/10.1016/j.polar.2021.100732 bah unknown Zenodo https://zenodo.org/communities/nunataryuk https://zenodo.org/communities/eu https://doi.org/10.1016/j.polar.2021.100732 oai:zenodo.org:5221400 info:eu-repo/semantics/openAccess Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode Soil temperatureArctic coastal erosionThermodenudationPermafrost thawing info:eu-repo/semantics/article 2021 ftzenodo https://doi.org/10.1016/j.polar.2021.100732 2024-07-26T08:33:25Z Abstract 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. Article in Journal/Newspaper Baydaratskaya bay Kara Sea permafrost Zenodo Polar Science 30 100732
institution Open Polar
collection Zenodo
op_collection_id ftzenodo
language unknown
topic Soil temperatureArctic coastal erosionThermodenudationPermafrost thawing
spellingShingle Soil temperatureArctic coastal erosionThermodenudationPermafrost thawing
Islam, Mohammad Akhsanul
Lubbad, Raed
Modelling the seasonal variations of soil temperatures in the Arctic coasts
topic_facet Soil temperatureArctic coastal erosionThermodenudationPermafrost thawing
description Abstract 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.
format Article in Journal/Newspaper
author Islam, Mohammad Akhsanul
Lubbad, Raed
author_facet Islam, Mohammad Akhsanul
Lubbad, Raed
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 Zenodo
publishDate 2021
url https://doi.org/10.1016/j.polar.2021.100732
genre Baydaratskaya bay
Kara Sea
permafrost
genre_facet Baydaratskaya bay
Kara Sea
permafrost
op_relation https://zenodo.org/communities/nunataryuk
https://zenodo.org/communities/eu
https://doi.org/10.1016/j.polar.2021.100732
oai:zenodo.org:5221400
op_rights info:eu-repo/semantics/openAccess
Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
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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