CO 2 and CH 4 exchanges between moist moss tundra and atmosphere on Kapp Linné, Svalbard
We measured CO 2 and CH 4 fluxes using chambers and eddy covariance (only CO 2 ) from a moist moss tundra in Svalbard. The average net ecosystem exchange (NEE) during the summer (9 June–31 August) was negative (sink), with − 0.139 ± 0.032 µ mol m −2 s −1 corresponding to − 11.8 g C m −2 for the whol...
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Copernicus Publications
2022
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Online Access: | https://doi.org/10.5194/bg-19-3921-2022 https://doaj.org/article/2817d9856a514d59ba0e7c9bcd60dc4a |
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ftdoajarticles:oai:doaj.org/article:2817d9856a514d59ba0e7c9bcd60dc4a 2023-05-15T15:17:59+02:00 CO 2 and CH 4 exchanges between moist moss tundra and atmosphere on Kapp Linné, Svalbard A. Lindroth N. Pirk I. S. Jónsdóttir C. Stiegler L. Klemedtsson M. B. Nilsson 2022-08-01T00:00:00Z https://doi.org/10.5194/bg-19-3921-2022 https://doaj.org/article/2817d9856a514d59ba0e7c9bcd60dc4a EN eng Copernicus Publications https://bg.copernicus.org/articles/19/3921/2022/bg-19-3921-2022.pdf https://doaj.org/toc/1726-4170 https://doaj.org/toc/1726-4189 doi:10.5194/bg-19-3921-2022 1726-4170 1726-4189 https://doaj.org/article/2817d9856a514d59ba0e7c9bcd60dc4a Biogeosciences, Vol 19, Pp 3921-3934 (2022) Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 article 2022 ftdoajarticles https://doi.org/10.5194/bg-19-3921-2022 2022-12-31T00:49:16Z We measured CO 2 and CH 4 fluxes using chambers and eddy covariance (only CO 2 ) from a moist moss tundra in Svalbard. The average net ecosystem exchange (NEE) during the summer (9 June–31 August) was negative (sink), with − 0.139 ± 0.032 µ mol m −2 s −1 corresponding to − 11.8 g C m −2 for the whole summer. The cumulated NEE over the whole growing season (day no. 160 to 284) was − 2.5 g C m −2 . The CH 4 flux during the summer period showed a large spatial and temporal variability. The mean value of all 214 samples was 0.000511 ± 0.000315 µ mol m −2 s −1 , which corresponds to a growing season estimate of 0.04 to 0.16 g CH 4 m −2 . Thus, we find that this moss tundra ecosystem is closely in balance with the atmosphere during the growing season when regarding exchanges of CO 2 and CH 4 . The sink of CO 2 and the source of CH 4 are small in comparison with other tundra ecosystems in the high Arctic. Air temperature, soil moisture and the greenness index contributed significantly to explaining the variation in ecosystem respiration ( R eco ), while active layer depth, soil moisture and the greenness index were the variables that best explained CH 4 emissions. An estimate of temperature sensitivity of R eco and gross primary productivity (GPP) showed that the sensitivity is slightly higher for GPP than for R eco in the interval 0–4.5 ∘ C; thereafter, the difference is small up to about 6 ∘ C and then begins to rise rapidly for R eco . The consequence of this, for a small increase in air temperature of 1 ∘ (all other variables assumed unchanged), was that the respiration increased more than photosynthesis turning the small sink into a small source (4.5 g C m −2 ) during the growing season. Thus, we cannot rule out that the reason why the moss tundra is close to balance today is an effect of the warming that has already taken place in Svalbard. Article in Journal/Newspaper Arctic Svalbard Tundra Directory of Open Access Journals: DOAJ Articles Arctic Kapp Linné ENVELOPE(13.621,13.621,78.063,78.063) Svalbard Biogeosciences 19 16 3921 3934 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
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 A. Lindroth N. Pirk I. S. Jónsdóttir C. Stiegler L. Klemedtsson M. B. Nilsson CO 2 and CH 4 exchanges between moist moss tundra and atmosphere on Kapp Linné, Svalbard |
topic_facet |
Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 |
description |
We measured CO 2 and CH 4 fluxes using chambers and eddy covariance (only CO 2 ) from a moist moss tundra in Svalbard. The average net ecosystem exchange (NEE) during the summer (9 June–31 August) was negative (sink), with − 0.139 ± 0.032 µ mol m −2 s −1 corresponding to − 11.8 g C m −2 for the whole summer. The cumulated NEE over the whole growing season (day no. 160 to 284) was − 2.5 g C m −2 . The CH 4 flux during the summer period showed a large spatial and temporal variability. The mean value of all 214 samples was 0.000511 ± 0.000315 µ mol m −2 s −1 , which corresponds to a growing season estimate of 0.04 to 0.16 g CH 4 m −2 . Thus, we find that this moss tundra ecosystem is closely in balance with the atmosphere during the growing season when regarding exchanges of CO 2 and CH 4 . The sink of CO 2 and the source of CH 4 are small in comparison with other tundra ecosystems in the high Arctic. Air temperature, soil moisture and the greenness index contributed significantly to explaining the variation in ecosystem respiration ( R eco ), while active layer depth, soil moisture and the greenness index were the variables that best explained CH 4 emissions. An estimate of temperature sensitivity of R eco and gross primary productivity (GPP) showed that the sensitivity is slightly higher for GPP than for R eco in the interval 0–4.5 ∘ C; thereafter, the difference is small up to about 6 ∘ C and then begins to rise rapidly for R eco . The consequence of this, for a small increase in air temperature of 1 ∘ (all other variables assumed unchanged), was that the respiration increased more than photosynthesis turning the small sink into a small source (4.5 g C m −2 ) during the growing season. Thus, we cannot rule out that the reason why the moss tundra is close to balance today is an effect of the warming that has already taken place in Svalbard. |
format |
Article in Journal/Newspaper |
author |
A. Lindroth N. Pirk I. S. Jónsdóttir C. Stiegler L. Klemedtsson M. B. Nilsson |
author_facet |
A. Lindroth N. Pirk I. S. Jónsdóttir C. Stiegler L. Klemedtsson M. B. Nilsson |
author_sort |
A. Lindroth |
title |
CO 2 and CH 4 exchanges between moist moss tundra and atmosphere on Kapp Linné, Svalbard |
title_short |
CO 2 and CH 4 exchanges between moist moss tundra and atmosphere on Kapp Linné, Svalbard |
title_full |
CO 2 and CH 4 exchanges between moist moss tundra and atmosphere on Kapp Linné, Svalbard |
title_fullStr |
CO 2 and CH 4 exchanges between moist moss tundra and atmosphere on Kapp Linné, Svalbard |
title_full_unstemmed |
CO 2 and CH 4 exchanges between moist moss tundra and atmosphere on Kapp Linné, Svalbard |
title_sort |
co 2 and ch 4 exchanges between moist moss tundra and atmosphere on kapp linné, svalbard |
publisher |
Copernicus Publications |
publishDate |
2022 |
url |
https://doi.org/10.5194/bg-19-3921-2022 https://doaj.org/article/2817d9856a514d59ba0e7c9bcd60dc4a |
long_lat |
ENVELOPE(13.621,13.621,78.063,78.063) |
geographic |
Arctic Kapp Linné Svalbard |
geographic_facet |
Arctic Kapp Linné Svalbard |
genre |
Arctic Svalbard Tundra |
genre_facet |
Arctic Svalbard Tundra |
op_source |
Biogeosciences, Vol 19, Pp 3921-3934 (2022) |
op_relation |
https://bg.copernicus.org/articles/19/3921/2022/bg-19-3921-2022.pdf https://doaj.org/toc/1726-4170 https://doaj.org/toc/1726-4189 doi:10.5194/bg-19-3921-2022 1726-4170 1726-4189 https://doaj.org/article/2817d9856a514d59ba0e7c9bcd60dc4a |
op_doi |
https://doi.org/10.5194/bg-19-3921-2022 |
container_title |
Biogeosciences |
container_volume |
19 |
container_issue |
16 |
container_start_page |
3921 |
op_container_end_page |
3934 |
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1766348224539394048 |