Optical and radar Earth observation data for upscaling methane emissions linked to permafrost degradation in sub-Arctic peatlands in northern Sweden
Permafrost thaw in Arctic regions is increasing methane (CH 4 ) emissions into the atmosphere, but quantification of such emissions is difficult given the large and remote areas impacted. Hence, Earth observation (EO) data are critical for assessing permafrost thaw, associated ecosystem change and i...
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ftdoajarticles:oai:doaj.org/article:7f2eb48c0c0b4150884df0ed008981a1 2023-11-12T04:12:58+01:00 Optical and radar Earth observation data for upscaling methane emissions linked to permafrost degradation in sub-Arctic peatlands in northern Sweden S. Sjögersten M. Ledger M. Siewert B. de la Barreda-Bautista A. Sowter D. Gee G. Foody D. S. Boyd 2023-10-01T00:00:00Z https://doi.org/10.5194/bg-20-4221-2023 https://doaj.org/article/7f2eb48c0c0b4150884df0ed008981a1 EN eng Copernicus Publications https://bg.copernicus.org/articles/20/4221/2023/bg-20-4221-2023.pdf https://doaj.org/toc/1726-4170 https://doaj.org/toc/1726-4189 doi:10.5194/bg-20-4221-2023 1726-4170 1726-4189 https://doaj.org/article/7f2eb48c0c0b4150884df0ed008981a1 Biogeosciences, Vol 20, Pp 4221-4239 (2023) Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 article 2023 ftdoajarticles https://doi.org/10.5194/bg-20-4221-2023 2023-10-22T00:42:48Z Permafrost thaw in Arctic regions is increasing methane (CH 4 ) emissions into the atmosphere, but quantification of such emissions is difficult given the large and remote areas impacted. Hence, Earth observation (EO) data are critical for assessing permafrost thaw, associated ecosystem change and increased CH 4 emissions. Often extrapolation from field measurements using EO is the approach employed. However, there are key challenges to consider. Landscape CH 4 emissions result from a complex local-scale mixture of micro-topographies and vegetation types that support widely differing CH 4 emissions, and it is difficult to detect the initial stages of permafrost degradation before vegetation transitions have occurred. This study considers the use of a combination of ultra-high-resolution unoccupied aerial vehicle (UAV) data and Sentinel-1 and Sentinel-2 data to extrapolate field measurements of CH 4 emissions from a set of vegetation types which capture the local variation in vegetation on degrading palsa wetlands. We show that the ultra-high-resolution UAV data can map spatial variation in vegetation relevant to variation in CH 4 emissions and extrapolate these across the wider landscape. We further show how this can be integrated with Sentinel-1 and Sentinel-2 data. By way of a soft classification and simple correction of misclassification bias of a hard classification, the output vegetation mapping and subsequent extrapolation of CH 4 emissions closely matched the results generated using the UAV data. Interferometric synthetic-aperture radar (InSAR) assessment of subsidence together with the vegetation classification suggested that high subsidence rates of palsa wetland can be used to quantify areas at risk of increased CH 4 emissions. The transition of a 50 ha area currently experiencing subsidence to fen vegetation is estimated to increase emissions from 116 kg CH 4 per season to emissions as high as 6500 to 13 000 kg CH 4 per season. The key outcome from this study is that a combination of high- and ... Article in Journal/Newspaper Arctic Northern Sweden palsa permafrost Directory of Open Access Journals: DOAJ Articles Arctic Biogeosciences 20 20 4221 4239 |
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Directory of Open Access Journals: DOAJ Articles |
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ftdoajarticles |
language |
English |
topic |
Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 |
spellingShingle |
Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 S. Sjögersten M. Ledger M. Siewert B. de la Barreda-Bautista A. Sowter D. Gee G. Foody D. S. Boyd Optical and radar Earth observation data for upscaling methane emissions linked to permafrost degradation in sub-Arctic peatlands in northern Sweden |
topic_facet |
Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 |
description |
Permafrost thaw in Arctic regions is increasing methane (CH 4 ) emissions into the atmosphere, but quantification of such emissions is difficult given the large and remote areas impacted. Hence, Earth observation (EO) data are critical for assessing permafrost thaw, associated ecosystem change and increased CH 4 emissions. Often extrapolation from field measurements using EO is the approach employed. However, there are key challenges to consider. Landscape CH 4 emissions result from a complex local-scale mixture of micro-topographies and vegetation types that support widely differing CH 4 emissions, and it is difficult to detect the initial stages of permafrost degradation before vegetation transitions have occurred. This study considers the use of a combination of ultra-high-resolution unoccupied aerial vehicle (UAV) data and Sentinel-1 and Sentinel-2 data to extrapolate field measurements of CH 4 emissions from a set of vegetation types which capture the local variation in vegetation on degrading palsa wetlands. We show that the ultra-high-resolution UAV data can map spatial variation in vegetation relevant to variation in CH 4 emissions and extrapolate these across the wider landscape. We further show how this can be integrated with Sentinel-1 and Sentinel-2 data. By way of a soft classification and simple correction of misclassification bias of a hard classification, the output vegetation mapping and subsequent extrapolation of CH 4 emissions closely matched the results generated using the UAV data. Interferometric synthetic-aperture radar (InSAR) assessment of subsidence together with the vegetation classification suggested that high subsidence rates of palsa wetland can be used to quantify areas at risk of increased CH 4 emissions. The transition of a 50 ha area currently experiencing subsidence to fen vegetation is estimated to increase emissions from 116 kg CH 4 per season to emissions as high as 6500 to 13 000 kg CH 4 per season. The key outcome from this study is that a combination of high- and ... |
format |
Article in Journal/Newspaper |
author |
S. Sjögersten M. Ledger M. Siewert B. de la Barreda-Bautista A. Sowter D. Gee G. Foody D. S. Boyd |
author_facet |
S. Sjögersten M. Ledger M. Siewert B. de la Barreda-Bautista A. Sowter D. Gee G. Foody D. S. Boyd |
author_sort |
S. Sjögersten |
title |
Optical and radar Earth observation data for upscaling methane emissions linked to permafrost degradation in sub-Arctic peatlands in northern Sweden |
title_short |
Optical and radar Earth observation data for upscaling methane emissions linked to permafrost degradation in sub-Arctic peatlands in northern Sweden |
title_full |
Optical and radar Earth observation data for upscaling methane emissions linked to permafrost degradation in sub-Arctic peatlands in northern Sweden |
title_fullStr |
Optical and radar Earth observation data for upscaling methane emissions linked to permafrost degradation in sub-Arctic peatlands in northern Sweden |
title_full_unstemmed |
Optical and radar Earth observation data for upscaling methane emissions linked to permafrost degradation in sub-Arctic peatlands in northern Sweden |
title_sort |
optical and radar earth observation data for upscaling methane emissions linked to permafrost degradation in sub-arctic peatlands in northern sweden |
publisher |
Copernicus Publications |
publishDate |
2023 |
url |
https://doi.org/10.5194/bg-20-4221-2023 https://doaj.org/article/7f2eb48c0c0b4150884df0ed008981a1 |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic Northern Sweden palsa permafrost |
genre_facet |
Arctic Northern Sweden palsa permafrost |
op_source |
Biogeosciences, Vol 20, Pp 4221-4239 (2023) |
op_relation |
https://bg.copernicus.org/articles/20/4221/2023/bg-20-4221-2023.pdf https://doaj.org/toc/1726-4170 https://doaj.org/toc/1726-4189 doi:10.5194/bg-20-4221-2023 1726-4170 1726-4189 https://doaj.org/article/7f2eb48c0c0b4150884df0ed008981a1 |
op_doi |
https://doi.org/10.5194/bg-20-4221-2023 |
container_title |
Biogeosciences |
container_volume |
20 |
container_issue |
20 |
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4221 |
op_container_end_page |
4239 |
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1782331206532071424 |