Spatial variation in landscape-level CO 2 and CH 4 fluxes from arctic coastal tundra: influence from vegetation, wetness, and the thaw lake cycle
Regional quantification of arctic CO 2 and CH 4 fluxes remains difficult due to high landscape heterogeneity coupled with a sparse measurement network. Most of the arctic coastal tundra near Barrow, Alaska is part of the thaw lake cycle, which includes current thaw lakes and a 5500-year chronosequen...
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ftopenunivgb:oai:oro.open.ac.uk:38751 2023-06-11T04:07:33+02:00 Spatial variation in landscape-level CO 2 and CH 4 fluxes from arctic coastal tundra: influence from vegetation, wetness, and the thaw lake cycle Sturtevant, Cove S. Oechel, Walter C. 2013 https://oro.open.ac.uk/38751/ https://doi.org/10.1111/gcb.12247 unknown Sturtevant, Cove S. and Oechel, Walter C. <http://oro.open.ac.uk/view/person/wco5.html> (2013). Spatial variation in landscape-level CO2and CH4fluxes from arctic coastal tundra: influence from vegetation, wetness, and the thaw lake cycle. Global Change Biology, 19(9) pp. 2853–2866. Journal Item None PeerReviewed 2013 ftopenunivgb https://doi.org/10.1111/gcb.12247 2023-05-28T05:50:34Z Regional quantification of arctic CO 2 and CH 4 fluxes remains difficult due to high landscape heterogeneity coupled with a sparse measurement network. Most of the arctic coastal tundra near Barrow, Alaska is part of the thaw lake cycle, which includes current thaw lakes and a 5500-year chronosequence of vegetated thaw lake basins. However, spatial variability in carbon fluxes from these features remains grossly understudied. Here, we present an analysis of whole-ecosystem CO 2 and CH 4 fluxes from 20 thaw lake cycle features during the 2011 growing season. We found that the thaw lake cycle was largely responsible for spatial variation in CO 2 flux, mostly due to its control on gross primary productivity (GPP). Current lakes were significant CO 2 sources that varied little. Vegetated basins showed declining GPP and CO 2 sink with age (R 2 = 67% and 57%, respectively). CH 4 fluxes measured from a subset of 12 vegetated basins showed no relationship with age or CO 2 flux components. Instead, higher CH 4 fluxes were related to greater landscape wetness (R 2 = 57%) and thaw depth (additional R 2 = 28%). Spatial variation in CO 2 and CH 4 fluxes had good satellite remote sensing indicators, and we estimated the region to be a small CO 2 sink of -4.9 ± 2.4 (SE) g C m -2 between 11 June and 25 August, which was countered by a CH 4 source of 2.1 ± 0.2 (SE) g C m -2 . Results from our scaling exercise showed that developing or validating regional estimates based on single tower sites can result in significant bias, on average by a factor 4 for CO 2 flux and 30% for CH 4 flux. Although our results are specific to the Arctic Coastal Plain of Alaska, the degree of landscape-scale variability, large-scale controls on carbon exchange, and implications for regional estimation seen here likely have wide relevance to other arctic landscapes. Article in Journal/Newspaper Arctic Arctic Barrow Tundra Alaska The Open University: Open Research Online (ORO) Arctic Global Change Biology 19 9 2853 2866 |
institution |
Open Polar |
collection |
The Open University: Open Research Online (ORO) |
op_collection_id |
ftopenunivgb |
language |
unknown |
description |
Regional quantification of arctic CO 2 and CH 4 fluxes remains difficult due to high landscape heterogeneity coupled with a sparse measurement network. Most of the arctic coastal tundra near Barrow, Alaska is part of the thaw lake cycle, which includes current thaw lakes and a 5500-year chronosequence of vegetated thaw lake basins. However, spatial variability in carbon fluxes from these features remains grossly understudied. Here, we present an analysis of whole-ecosystem CO 2 and CH 4 fluxes from 20 thaw lake cycle features during the 2011 growing season. We found that the thaw lake cycle was largely responsible for spatial variation in CO 2 flux, mostly due to its control on gross primary productivity (GPP). Current lakes were significant CO 2 sources that varied little. Vegetated basins showed declining GPP and CO 2 sink with age (R 2 = 67% and 57%, respectively). CH 4 fluxes measured from a subset of 12 vegetated basins showed no relationship with age or CO 2 flux components. Instead, higher CH 4 fluxes were related to greater landscape wetness (R 2 = 57%) and thaw depth (additional R 2 = 28%). Spatial variation in CO 2 and CH 4 fluxes had good satellite remote sensing indicators, and we estimated the region to be a small CO 2 sink of -4.9 ± 2.4 (SE) g C m -2 between 11 June and 25 August, which was countered by a CH 4 source of 2.1 ± 0.2 (SE) g C m -2 . Results from our scaling exercise showed that developing or validating regional estimates based on single tower sites can result in significant bias, on average by a factor 4 for CO 2 flux and 30% for CH 4 flux. Although our results are specific to the Arctic Coastal Plain of Alaska, the degree of landscape-scale variability, large-scale controls on carbon exchange, and implications for regional estimation seen here likely have wide relevance to other arctic landscapes. |
format |
Article in Journal/Newspaper |
author |
Sturtevant, Cove S. Oechel, Walter C. |
spellingShingle |
Sturtevant, Cove S. Oechel, Walter C. Spatial variation in landscape-level CO 2 and CH 4 fluxes from arctic coastal tundra: influence from vegetation, wetness, and the thaw lake cycle |
author_facet |
Sturtevant, Cove S. Oechel, Walter C. |
author_sort |
Sturtevant, Cove S. |
title |
Spatial variation in landscape-level CO 2 and CH 4 fluxes from arctic coastal tundra: influence from vegetation, wetness, and the thaw lake cycle |
title_short |
Spatial variation in landscape-level CO 2 and CH 4 fluxes from arctic coastal tundra: influence from vegetation, wetness, and the thaw lake cycle |
title_full |
Spatial variation in landscape-level CO 2 and CH 4 fluxes from arctic coastal tundra: influence from vegetation, wetness, and the thaw lake cycle |
title_fullStr |
Spatial variation in landscape-level CO 2 and CH 4 fluxes from arctic coastal tundra: influence from vegetation, wetness, and the thaw lake cycle |
title_full_unstemmed |
Spatial variation in landscape-level CO 2 and CH 4 fluxes from arctic coastal tundra: influence from vegetation, wetness, and the thaw lake cycle |
title_sort |
spatial variation in landscape-level co 2 and ch 4 fluxes from arctic coastal tundra: influence from vegetation, wetness, and the thaw lake cycle |
publishDate |
2013 |
url |
https://oro.open.ac.uk/38751/ https://doi.org/10.1111/gcb.12247 |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic Arctic Barrow Tundra Alaska |
genre_facet |
Arctic Arctic Barrow Tundra Alaska |
op_relation |
Sturtevant, Cove S. and Oechel, Walter C. <http://oro.open.ac.uk/view/person/wco5.html> (2013). Spatial variation in landscape-level CO2and CH4fluxes from arctic coastal tundra: influence from vegetation, wetness, and the thaw lake cycle. Global Change Biology, 19(9) pp. 2853–2866. |
op_doi |
https://doi.org/10.1111/gcb.12247 |
container_title |
Global Change Biology |
container_volume |
19 |
container_issue |
9 |
container_start_page |
2853 |
op_container_end_page |
2866 |
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1768380718867546112 |