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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Published in:Arctic Science
Main Authors: June Skeeter, Andreas Christen, Greg Henry
Format: Article in Journal/Newspaper
Language:English
French
Published: Canadian Science Publishing 2023
Subjects:
Online Access:https://doi.org/10.1139/as-2022-0033
https://doaj.org/article/c0642f7493c2470aacaaf0b05682f0a7
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spelling 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
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