Diurnal and seasonal variations of tundra CO2 emissions in a polygonal peatland near Salluit, Nunavik, Canada
Polygonal peatlands are carbon-rich permafrost ecosystems that will likely be significantly affected by climate change. However, studies are often constrained to one measurement per day, which impedes assessments of the temporal variability in carbon fluxes. For this reason, we measured ecosystem re...
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ftunivtoronto:oai:localhost:1807/79486 2023-05-15T17:57:33+02:00 Diurnal and seasonal variations of tundra CO2 emissions in a polygonal peatland near Salluit, Nunavik, Canada Gagnon, Samuel Allard, Michel Nicosia, Aurélien 2017-06-26 http://hdl.handle.net/1807/79486 http://www.nrcresearchpress.com/doi/abs/10.1139/AS-2016-0045 unknown NRC Research Press (a division of Canadian Science Publishing) N http://hdl.handle.net/1807/79486 http://www.nrcresearchpress.com/doi/abs/10.1139/AS-2016-0045 Article 2017 ftunivtoronto 2020-06-17T12:07:13Z Polygonal peatlands are carbon-rich permafrost ecosystems that will likely be significantly affected by climate change. However, studies are often constrained to one measurement per day, which impedes assessments of the temporal variability in carbon fluxes. For this reason, we measured ecosystem respiration (ER) of CO2 in a polygonal peatland underlain by continuous permafrost over an entire growing season to determine the effects of temperature and water table depth on the temporal variability of ER. We used four automated closed chambers to measure ER under varying temperature and soil moisture regimes. Temporal variability was approximately the same for the four plots, both on a diurnal and seasonal scale. Both diurnal and seasonal variations in ER were strongly controlled by changes in soil surface temperature. Fluctuations of the water table depth associated with important rainfall events was also an important factor affecting ER on the seasonal scale. We found that water table level fluctuations below 20-25 cm did not significantly affect ER and that most soil respiration took place in the top 10 cm, likely in the surface 2 cm. Our results highlight the importance of monitoring future changes in tundra hydrology, which will determine the depth of organic matter available for aerobic decomposition. The accepted manuscript in pdf format is listed with the files at the bottom of this page. The presentation of the authors' names and (or) special characters in the title of the manuscript may differ slightly between what is listed on this page and what is listed in the pdf file of the accepted manuscript; that in the pdf file of the accepted manuscript is what was submitted by the author. Article in Journal/Newspaper permafrost Salluit Tundra Nunavik University of Toronto: Research Repository T-Space Canada Nunavik Salluit ENVELOPE(-75.643,-75.643,62.204,62.204) |
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Open Polar |
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University of Toronto: Research Repository T-Space |
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ftunivtoronto |
language |
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description |
Polygonal peatlands are carbon-rich permafrost ecosystems that will likely be significantly affected by climate change. However, studies are often constrained to one measurement per day, which impedes assessments of the temporal variability in carbon fluxes. For this reason, we measured ecosystem respiration (ER) of CO2 in a polygonal peatland underlain by continuous permafrost over an entire growing season to determine the effects of temperature and water table depth on the temporal variability of ER. We used four automated closed chambers to measure ER under varying temperature and soil moisture regimes. Temporal variability was approximately the same for the four plots, both on a diurnal and seasonal scale. Both diurnal and seasonal variations in ER were strongly controlled by changes in soil surface temperature. Fluctuations of the water table depth associated with important rainfall events was also an important factor affecting ER on the seasonal scale. We found that water table level fluctuations below 20-25 cm did not significantly affect ER and that most soil respiration took place in the top 10 cm, likely in the surface 2 cm. Our results highlight the importance of monitoring future changes in tundra hydrology, which will determine the depth of organic matter available for aerobic decomposition. The accepted manuscript in pdf format is listed with the files at the bottom of this page. The presentation of the authors' names and (or) special characters in the title of the manuscript may differ slightly between what is listed on this page and what is listed in the pdf file of the accepted manuscript; that in the pdf file of the accepted manuscript is what was submitted by the author. |
format |
Article in Journal/Newspaper |
author |
Gagnon, Samuel Allard, Michel Nicosia, Aurélien |
spellingShingle |
Gagnon, Samuel Allard, Michel Nicosia, Aurélien Diurnal and seasonal variations of tundra CO2 emissions in a polygonal peatland near Salluit, Nunavik, Canada |
author_facet |
Gagnon, Samuel Allard, Michel Nicosia, Aurélien |
author_sort |
Gagnon, Samuel |
title |
Diurnal and seasonal variations of tundra CO2 emissions in a polygonal peatland near Salluit, Nunavik, Canada |
title_short |
Diurnal and seasonal variations of tundra CO2 emissions in a polygonal peatland near Salluit, Nunavik, Canada |
title_full |
Diurnal and seasonal variations of tundra CO2 emissions in a polygonal peatland near Salluit, Nunavik, Canada |
title_fullStr |
Diurnal and seasonal variations of tundra CO2 emissions in a polygonal peatland near Salluit, Nunavik, Canada |
title_full_unstemmed |
Diurnal and seasonal variations of tundra CO2 emissions in a polygonal peatland near Salluit, Nunavik, Canada |
title_sort |
diurnal and seasonal variations of tundra co2 emissions in a polygonal peatland near salluit, nunavik, canada |
publisher |
NRC Research Press (a division of Canadian Science Publishing) |
publishDate |
2017 |
url |
http://hdl.handle.net/1807/79486 http://www.nrcresearchpress.com/doi/abs/10.1139/AS-2016-0045 |
long_lat |
ENVELOPE(-75.643,-75.643,62.204,62.204) |
geographic |
Canada Nunavik Salluit |
geographic_facet |
Canada Nunavik Salluit |
genre |
permafrost Salluit Tundra Nunavik |
genre_facet |
permafrost Salluit Tundra Nunavik |
op_relation |
N http://hdl.handle.net/1807/79486 http://www.nrcresearchpress.com/doi/abs/10.1139/AS-2016-0045 |
_version_ |
1766166014572101632 |