Satellite data in thermal range for natural and technogenic ecosystems monitoring

A method for recovery monitoring in post-fire and post-technogenic landscapes was proposed based on satellite data in a wide spectral range, including the infrared band data. A decrease in the spectral surface albedo in post-fire areas, caused by the destruction of on-ground vegetation, provokes exc...

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Published in:E3S Web of Conferences
Main Authors: Yakimov Nikita, Ponomarev Evgenii, Ponomareva Tatiana
Format: Article in Journal/Newspaper
Language:English
French
Published: EDP Sciences 2021
Subjects:
Online Access:https://doi.org/10.1051/e3sconf/202133302017
https://doaj.org/article/972609bbdeb449c785006ef963aae924
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spelling ftdoajarticles:oai:doaj.org/article:972609bbdeb449c785006ef963aae924 2023-05-15T17:57:53+02:00 Satellite data in thermal range for natural and technogenic ecosystems monitoring Yakimov Nikita Ponomarev Evgenii Ponomareva Tatiana 2021-01-01T00:00:00Z https://doi.org/10.1051/e3sconf/202133302017 https://doaj.org/article/972609bbdeb449c785006ef963aae924 EN FR eng fre EDP Sciences https://www.e3s-conferences.org/articles/e3sconf/pdf/2021/109/e3sconf_rpers2021_02017.pdf https://doaj.org/toc/2267-1242 2267-1242 doi:10.1051/e3sconf/202133302017 https://doaj.org/article/972609bbdeb449c785006ef963aae924 E3S Web of Conferences, Vol 333, p 02017 (2021) Environmental sciences GE1-350 article 2021 ftdoajarticles https://doi.org/10.1051/e3sconf/202133302017 2022-12-31T15:09:44Z A method for recovery monitoring in post-fire and post-technogenic landscapes was proposed based on satellite data in a wide spectral range, including the infrared band data. A decrease in the spectral surface albedo in post-fire areas, caused by the destruction of on-ground vegetation, provokes excessive heating of the surface and upper soil layer. Surface thermal anomalies were evaluated under conditions of changes in the heat-insulating properties of vegetation and ground cover. The relative temperature anomalies in post-fire plots (overestimation up to 30% compared to non-disturbed territory) are typical for permafrost conditions of Siberia. Similar process was recorded for both natural (post-fire) and post-technogenic landscapes. Within 22 years after the fire, thermal insulation properties of the vegetation cover were restored. Thus, the relative temperature anomaly (of 3±1%) has reached the background value. In post-technogenic plots, conditions are more “contrast” compared to the background, and restoration of the thermal regime takes significantly longer (>60 years). “Neo-technogenic ecosystems” with specific soil thermal regimes compared to the background ones are formed both for reclaimed and for non-reclaimed post-technogenic plots. On average, surface temperature has overestimated at least by 10–15% in post-technogenic plots compared to non-disturbed territory. Article in Journal/Newspaper permafrost Siberia Directory of Open Access Journals: DOAJ Articles E3S Web of Conferences 333 02017
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
French
topic Environmental sciences
GE1-350
spellingShingle Environmental sciences
GE1-350
Yakimov Nikita
Ponomarev Evgenii
Ponomareva Tatiana
Satellite data in thermal range for natural and technogenic ecosystems monitoring
topic_facet Environmental sciences
GE1-350
description A method for recovery monitoring in post-fire and post-technogenic landscapes was proposed based on satellite data in a wide spectral range, including the infrared band data. A decrease in the spectral surface albedo in post-fire areas, caused by the destruction of on-ground vegetation, provokes excessive heating of the surface and upper soil layer. Surface thermal anomalies were evaluated under conditions of changes in the heat-insulating properties of vegetation and ground cover. The relative temperature anomalies in post-fire plots (overestimation up to 30% compared to non-disturbed territory) are typical for permafrost conditions of Siberia. Similar process was recorded for both natural (post-fire) and post-technogenic landscapes. Within 22 years after the fire, thermal insulation properties of the vegetation cover were restored. Thus, the relative temperature anomaly (of 3±1%) has reached the background value. In post-technogenic plots, conditions are more “contrast” compared to the background, and restoration of the thermal regime takes significantly longer (>60 years). “Neo-technogenic ecosystems” with specific soil thermal regimes compared to the background ones are formed both for reclaimed and for non-reclaimed post-technogenic plots. On average, surface temperature has overestimated at least by 10–15% in post-technogenic plots compared to non-disturbed territory.
format Article in Journal/Newspaper
author Yakimov Nikita
Ponomarev Evgenii
Ponomareva Tatiana
author_facet Yakimov Nikita
Ponomarev Evgenii
Ponomareva Tatiana
author_sort Yakimov Nikita
title Satellite data in thermal range for natural and technogenic ecosystems monitoring
title_short Satellite data in thermal range for natural and technogenic ecosystems monitoring
title_full Satellite data in thermal range for natural and technogenic ecosystems monitoring
title_fullStr Satellite data in thermal range for natural and technogenic ecosystems monitoring
title_full_unstemmed Satellite data in thermal range for natural and technogenic ecosystems monitoring
title_sort satellite data in thermal range for natural and technogenic ecosystems monitoring
publisher EDP Sciences
publishDate 2021
url https://doi.org/10.1051/e3sconf/202133302017
https://doaj.org/article/972609bbdeb449c785006ef963aae924
genre permafrost
Siberia
genre_facet permafrost
Siberia
op_source E3S Web of Conferences, Vol 333, p 02017 (2021)
op_relation https://www.e3s-conferences.org/articles/e3sconf/pdf/2021/109/e3sconf_rpers2021_02017.pdf
https://doaj.org/toc/2267-1242
2267-1242
doi:10.1051/e3sconf/202133302017
https://doaj.org/article/972609bbdeb449c785006ef963aae924
op_doi https://doi.org/10.1051/e3sconf/202133302017
container_title E3S Web of Conferences
container_volume 333
container_start_page 02017
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