Modelling growing season carbon fluxes at a low-center polygon ecosystem in the Mackenzie River Delta
A temporal upscaling study was conducted to estimate net ecosystem exchange (NEE) of carbon dioxide and net methane exchange (NME) for a low-center polygon (LCP) ecosystem in the Mackenzie River Delta, for each of the 11 growing seasons (2009–2019). We used regression models to create a time series...
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Canadian Science Publishing
2023
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Online Access: | https://doi.org/10.1139/as-2022-0033 https://doaj.org/article/c0642f7493c2470aacaaf0b05682f0a7 |
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ftdoajarticles:oai:doaj.org/article:c0642f7493c2470aacaaf0b05682f0a7 2023-10-01T03:52:30+02:00 Modelling growing season carbon fluxes at a low-center polygon ecosystem in the Mackenzie River Delta June Skeeter Andreas Christen Greg Henry 2023-09-01T00:00:00Z https://doi.org/10.1139/as-2022-0033 https://doaj.org/article/c0642f7493c2470aacaaf0b05682f0a7 EN FR eng fre Canadian Science Publishing https://cdnsciencepub.com/doi/10.1139/as-2022-0033 https://doaj.org/toc/2368-7460 doi:10.1139/as-2022-0033 2368-7460 https://doaj.org/article/c0642f7493c2470aacaaf0b05682f0a7 Arctic Science, Vol 9, Iss 3, Pp 689-709 (2023) carbon fluxes polygonal tundra permafrost climate change machine learning Environmental sciences GE1-350 Environmental engineering TA170-171 article 2023 ftdoajarticles https://doi.org/10.1139/as-2022-0033 2023-09-03T00:48:51Z A temporal upscaling study was conducted to estimate net ecosystem exchange (NEE) of carbon dioxide and net methane exchange (NME) for a low-center polygon (LCP) ecosystem in the Mackenzie River Delta, for each of the 11 growing seasons (2009–2019). We used regression models to create a time series of flux drivers from in situ weather observations (2009–2019) combined with ERA5 reanalysis and satellite data. We then used neural networks that were trained and validated on a single growing season (2017) of eddy covariance data to model NEE and NME over each growing season. The study indicates growing season NEE was negative (net uptake) and NME was positive (net emission) in this LCP ecosystem. Cumulative carbon (C) uptake was estimated to be −46.7 g C m−2 (CI95% ± 45.3) per growing season, with methane emissions offsetting an average 5.6% of carbon dioxide uptake (in g C m−2) per growing season. High air temperatures (>15 °C) reduced daily CO2 uptake and cumulative NEE was positively correlated with mean air growing season temperatures. Cumulative NME was positively correlated with the length of the growing season. Our analysis suggests warmer climate conditions may reduce carbon uptake in this LCP ecosystem. Article in Journal/Newspaper Arctic Mackenzie river permafrost Tundra Directory of Open Access Journals: DOAJ Articles Mackenzie River Arctic Science |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English French |
topic |
carbon fluxes polygonal tundra permafrost climate change machine learning Environmental sciences GE1-350 Environmental engineering TA170-171 |
spellingShingle |
carbon fluxes polygonal tundra permafrost climate change machine learning Environmental sciences GE1-350 Environmental engineering TA170-171 June Skeeter Andreas Christen Greg Henry Modelling growing season carbon fluxes at a low-center polygon ecosystem in the Mackenzie River Delta |
topic_facet |
carbon fluxes polygonal tundra permafrost climate change machine learning Environmental sciences GE1-350 Environmental engineering TA170-171 |
description |
A temporal upscaling study was conducted to estimate net ecosystem exchange (NEE) of carbon dioxide and net methane exchange (NME) for a low-center polygon (LCP) ecosystem in the Mackenzie River Delta, for each of the 11 growing seasons (2009–2019). We used regression models to create a time series of flux drivers from in situ weather observations (2009–2019) combined with ERA5 reanalysis and satellite data. We then used neural networks that were trained and validated on a single growing season (2017) of eddy covariance data to model NEE and NME over each growing season. The study indicates growing season NEE was negative (net uptake) and NME was positive (net emission) in this LCP ecosystem. Cumulative carbon (C) uptake was estimated to be −46.7 g C m−2 (CI95% ± 45.3) per growing season, with methane emissions offsetting an average 5.6% of carbon dioxide uptake (in g C m−2) per growing season. High air temperatures (>15 °C) reduced daily CO2 uptake and cumulative NEE was positively correlated with mean air growing season temperatures. Cumulative NME was positively correlated with the length of the growing season. Our analysis suggests warmer climate conditions may reduce carbon uptake in this LCP ecosystem. |
format |
Article in Journal/Newspaper |
author |
June Skeeter Andreas Christen Greg Henry |
author_facet |
June Skeeter Andreas Christen Greg Henry |
author_sort |
June Skeeter |
title |
Modelling growing season carbon fluxes at a low-center polygon ecosystem in the Mackenzie River Delta |
title_short |
Modelling growing season carbon fluxes at a low-center polygon ecosystem in the Mackenzie River Delta |
title_full |
Modelling growing season carbon fluxes at a low-center polygon ecosystem in the Mackenzie River Delta |
title_fullStr |
Modelling growing season carbon fluxes at a low-center polygon ecosystem in the Mackenzie River Delta |
title_full_unstemmed |
Modelling growing season carbon fluxes at a low-center polygon ecosystem in the Mackenzie River Delta |
title_sort |
modelling growing season carbon fluxes at a low-center polygon ecosystem in the mackenzie river delta |
publisher |
Canadian Science Publishing |
publishDate |
2023 |
url |
https://doi.org/10.1139/as-2022-0033 https://doaj.org/article/c0642f7493c2470aacaaf0b05682f0a7 |
geographic |
Mackenzie River |
geographic_facet |
Mackenzie River |
genre |
Arctic Mackenzie river permafrost Tundra |
genre_facet |
Arctic Mackenzie river permafrost Tundra |
op_source |
Arctic Science, Vol 9, Iss 3, Pp 689-709 (2023) |
op_relation |
https://cdnsciencepub.com/doi/10.1139/as-2022-0033 https://doaj.org/toc/2368-7460 doi:10.1139/as-2022-0033 2368-7460 https://doaj.org/article/c0642f7493c2470aacaaf0b05682f0a7 |
op_doi |
https://doi.org/10.1139/as-2022-0033 |
container_title |
Arctic Science |
_version_ |
1778518657276575744 |