Thermal photogrammetry on a permafrost rock wall for the active layer monitoring

Permafrost and active layer models often cannot explain the high spatial variability, especially in heterogeneous environments like the mountainous regions due to their scarce resolution, paucity of climatic data and topographic details. In this study, we want to introduce a new application of the u...

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Published in:Science of The Total Environment
Main Authors: Ponti, Stefano, Girola, Irene, Guglielmin, Mauro
Format: Article in Journal/Newspaper
Language:English
Published: 2024
Subjects:
Online Access:https://hdl.handle.net/11383/2166832
https://doi.org/10.1016/j.scitotenv.2024.170391
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spelling ftuninsubriairis:oai:irinsubria.uninsubria.it:11383/2166832 2024-04-14T08:00:08+00:00 Thermal photogrammetry on a permafrost rock wall for the active layer monitoring Ponti, Stefano Girola, Irene Guglielmin, Mauro Ponti, Stefano Girola, Irene Guglielmin, Mauro 2024 ELETTRONICO https://hdl.handle.net/11383/2166832 https://doi.org/10.1016/j.scitotenv.2024.170391 eng eng info:eu-repo/semantics/altIdentifier/pmid/38281645 volume:917 firstpage:1 lastpage:15 numberofpages:15 journal:SCIENCE OF THE TOTAL ENVIRONMENT https://hdl.handle.net/11383/2166832 doi:10.1016/j.scitotenv.2024.170391 info:eu-repo/semantics/openAccess ALT modelling Permafrost Rock wall Thermal inertia Thermal photogrammetry info:eu-repo/semantics/article 2024 ftuninsubriairis https://doi.org/10.1016/j.scitotenv.2024.170391 2024-03-21T19:14:02Z Permafrost and active layer models often cannot explain the high spatial variability, especially in heterogeneous environments like the mountainous regions due to their scarce resolution, paucity of climatic data and topographic details. In this study, we want to introduce a new application of the unmanned aerial vehicle (UAV) in thermal photogrammetry to model the active layer thickness (ALT) of an alpine rock wall through the computation of the thermal inertia and compare the results with a widespread ALT model. On the Gran Zebrù South rock wall, 8 thermal UAV surveys has been conducted in 4 different summer days during 2021-2022 in order to have two 3D thermal models per day at different solar radiation inputs. By analyzing topographic data, visible imagery and the thermal models, the apparent thermal inertias (ATIs) have been converted into heat transfer coefficients (HTCs) and then into ALT of 2021 and 2022. These maps have been validated through the placement of thermistors at different elevations and with variable depths (2, 15 and 40 cm from the rock surface). The resulting ALT has been compared with the Stefan's solution and the alpine permafrost index map (APIM), which showed large underestimations and a noncorrespondence with permafrost occurrence. The average ALT increase of 29.3 cm from 2021 to 2022 has been discussed regarding permafrost formation/degradation future trend under the climatic change and potential risks of alpine areas. Article in Journal/Newspaper Active layer monitoring Active layer thickness permafrost IRInSubria - Institutional Repository Insubria (Università degli Studi dell’Insubria) Science of The Total Environment 917 170391
institution Open Polar
collection IRInSubria - Institutional Repository Insubria (Università degli Studi dell’Insubria)
op_collection_id ftuninsubriairis
language English
topic ALT modelling
Permafrost
Rock wall
Thermal inertia
Thermal photogrammetry
spellingShingle ALT modelling
Permafrost
Rock wall
Thermal inertia
Thermal photogrammetry
Ponti, Stefano
Girola, Irene
Guglielmin, Mauro
Thermal photogrammetry on a permafrost rock wall for the active layer monitoring
topic_facet ALT modelling
Permafrost
Rock wall
Thermal inertia
Thermal photogrammetry
description Permafrost and active layer models often cannot explain the high spatial variability, especially in heterogeneous environments like the mountainous regions due to their scarce resolution, paucity of climatic data and topographic details. In this study, we want to introduce a new application of the unmanned aerial vehicle (UAV) in thermal photogrammetry to model the active layer thickness (ALT) of an alpine rock wall through the computation of the thermal inertia and compare the results with a widespread ALT model. On the Gran Zebrù South rock wall, 8 thermal UAV surveys has been conducted in 4 different summer days during 2021-2022 in order to have two 3D thermal models per day at different solar radiation inputs. By analyzing topographic data, visible imagery and the thermal models, the apparent thermal inertias (ATIs) have been converted into heat transfer coefficients (HTCs) and then into ALT of 2021 and 2022. These maps have been validated through the placement of thermistors at different elevations and with variable depths (2, 15 and 40 cm from the rock surface). The resulting ALT has been compared with the Stefan's solution and the alpine permafrost index map (APIM), which showed large underestimations and a noncorrespondence with permafrost occurrence. The average ALT increase of 29.3 cm from 2021 to 2022 has been discussed regarding permafrost formation/degradation future trend under the climatic change and potential risks of alpine areas.
author2 Ponti, Stefano
Girola, Irene
Guglielmin, Mauro
format Article in Journal/Newspaper
author Ponti, Stefano
Girola, Irene
Guglielmin, Mauro
author_facet Ponti, Stefano
Girola, Irene
Guglielmin, Mauro
author_sort Ponti, Stefano
title Thermal photogrammetry on a permafrost rock wall for the active layer monitoring
title_short Thermal photogrammetry on a permafrost rock wall for the active layer monitoring
title_full Thermal photogrammetry on a permafrost rock wall for the active layer monitoring
title_fullStr Thermal photogrammetry on a permafrost rock wall for the active layer monitoring
title_full_unstemmed Thermal photogrammetry on a permafrost rock wall for the active layer monitoring
title_sort thermal photogrammetry on a permafrost rock wall for the active layer monitoring
publishDate 2024
url https://hdl.handle.net/11383/2166832
https://doi.org/10.1016/j.scitotenv.2024.170391
genre Active layer monitoring
Active layer thickness
permafrost
genre_facet Active layer monitoring
Active layer thickness
permafrost
op_relation info:eu-repo/semantics/altIdentifier/pmid/38281645
volume:917
firstpage:1
lastpage:15
numberofpages:15
journal:SCIENCE OF THE TOTAL ENVIRONMENT
https://hdl.handle.net/11383/2166832
doi:10.1016/j.scitotenv.2024.170391
op_rights info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.1016/j.scitotenv.2024.170391
container_title Science of The Total Environment
container_volume 917
container_start_page 170391
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