Modelling CH 4 emissions from arctic wetlands: effects of hydrological parameterization
This study compares the CH 4 fluxes from two arctic wetland sites of different annual temperatures during 2004 to 2006. The PEATLAND-VU model was used to simulate the emissions. The CH 4 module of PEATLAND-VU is based on the Walter-Heimann model. The first site is located in northeast Siberia, Indig...
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ftdoajarticles:oai:doaj.org/article:fa842e5d852b405084eecdff6caa6481 2023-05-15T12:59:56+02:00 Modelling CH 4 emissions from arctic wetlands: effects of hydrological parameterization T. C. Maximov P. M. Crill K. Bäckstrand T. R. Christensen A. Yurova M. Jackowicz-Korczynski J. van Huissteden A. M. R. Petrescu 2008-01-01T00:00:00Z https://doaj.org/article/fa842e5d852b405084eecdff6caa6481 EN eng Copernicus Publications http://www.biogeosciences.net/5/111/2008/bg-5-111-2008.pdf https://doaj.org/toc/1726-4170 https://doaj.org/toc/1726-4189 1726-4170 1726-4189 https://doaj.org/article/fa842e5d852b405084eecdff6caa6481 Biogeosciences, Vol 5, Iss 1, Pp 111-121 (2008) Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 article 2008 ftdoajarticles 2022-12-31T07:14:56Z This study compares the CH 4 fluxes from two arctic wetland sites of different annual temperatures during 2004 to 2006. The PEATLAND-VU model was used to simulate the emissions. The CH 4 module of PEATLAND-VU is based on the Walter-Heimann model. The first site is located in northeast Siberia, Indigirka lowlands, Kytalyk reserve (70° N, 147° E) in a continuous permafrost region with mean annual temperatures of −14.3°C. The other site is Stordalen mire in the eastern part of Lake Torneträsk (68° N, 19° E) ten kilometres east of Abisko, northern Sweden. It is located in a discontinuous permafrost region. Stordalen has a sub arctic climate with a mean annual temperature of −0.7°C. Model input consisted of observed temperature, precipitation and snow cover data. In all cases, modelled CH 4 emissions show a direct correlation between variations in water table and soil temperature variations. The differences in CH 4 emissions between the two sites are caused by different climate, hydrology, soil physical properties, vegetation type and NPP. For Kytalyk the simulated CH 4 fluxes show similar trends during the growing season, having average values for 2004 to 2006 between 1.29–2.09 mg CH 4 m −2 hr −1 . At Stordalen the simulated fluxes show a slightly lower average value for the same years (3.52 mg CH 4 m −2 hr −1 ) than the observed 4.7 mg CH 4 m −2 hr −1 . The effect of the longer growing season at Stordalen is simulated correctly. Our study shows that modelling of arctic CH 4 fluxes is improved by adding a relatively simple hydrological model that simulates the water table position from generic weather data. Our results support the generalization in literature that CH 4 fluxes in northern wetland are regulated more tightly by water table than temperature. Furthermore, parameter uncertainty at site level in wetland CH 4 process models is an important factor in large scale modelling of CH 4 fluxes. Article in Journal/Newspaper Abisko Arctic Northern Sweden permafrost Siberia Directory of Open Access Journals: DOAJ Articles Arctic Abisko ENVELOPE(18.829,18.829,68.349,68.349) Indigirka ENVELOPE(149.609,149.609,70.929,70.929) Stordalen ENVELOPE(7.337,7.337,62.510,62.510) Torneträsk ENVELOPE(18.861,18.861,68.392,68.392) |
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 T. C. Maximov P. M. Crill K. Bäckstrand T. R. Christensen A. Yurova M. Jackowicz-Korczynski J. van Huissteden A. M. R. Petrescu Modelling CH 4 emissions from arctic wetlands: effects of hydrological parameterization |
topic_facet |
Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 |
description |
This study compares the CH 4 fluxes from two arctic wetland sites of different annual temperatures during 2004 to 2006. The PEATLAND-VU model was used to simulate the emissions. The CH 4 module of PEATLAND-VU is based on the Walter-Heimann model. The first site is located in northeast Siberia, Indigirka lowlands, Kytalyk reserve (70° N, 147° E) in a continuous permafrost region with mean annual temperatures of −14.3°C. The other site is Stordalen mire in the eastern part of Lake Torneträsk (68° N, 19° E) ten kilometres east of Abisko, northern Sweden. It is located in a discontinuous permafrost region. Stordalen has a sub arctic climate with a mean annual temperature of −0.7°C. Model input consisted of observed temperature, precipitation and snow cover data. In all cases, modelled CH 4 emissions show a direct correlation between variations in water table and soil temperature variations. The differences in CH 4 emissions between the two sites are caused by different climate, hydrology, soil physical properties, vegetation type and NPP. For Kytalyk the simulated CH 4 fluxes show similar trends during the growing season, having average values for 2004 to 2006 between 1.29–2.09 mg CH 4 m −2 hr −1 . At Stordalen the simulated fluxes show a slightly lower average value for the same years (3.52 mg CH 4 m −2 hr −1 ) than the observed 4.7 mg CH 4 m −2 hr −1 . The effect of the longer growing season at Stordalen is simulated correctly. Our study shows that modelling of arctic CH 4 fluxes is improved by adding a relatively simple hydrological model that simulates the water table position from generic weather data. Our results support the generalization in literature that CH 4 fluxes in northern wetland are regulated more tightly by water table than temperature. Furthermore, parameter uncertainty at site level in wetland CH 4 process models is an important factor in large scale modelling of CH 4 fluxes. |
format |
Article in Journal/Newspaper |
author |
T. C. Maximov P. M. Crill K. Bäckstrand T. R. Christensen A. Yurova M. Jackowicz-Korczynski J. van Huissteden A. M. R. Petrescu |
author_facet |
T. C. Maximov P. M. Crill K. Bäckstrand T. R. Christensen A. Yurova M. Jackowicz-Korczynski J. van Huissteden A. M. R. Petrescu |
author_sort |
T. C. Maximov |
title |
Modelling CH 4 emissions from arctic wetlands: effects of hydrological parameterization |
title_short |
Modelling CH 4 emissions from arctic wetlands: effects of hydrological parameterization |
title_full |
Modelling CH 4 emissions from arctic wetlands: effects of hydrological parameterization |
title_fullStr |
Modelling CH 4 emissions from arctic wetlands: effects of hydrological parameterization |
title_full_unstemmed |
Modelling CH 4 emissions from arctic wetlands: effects of hydrological parameterization |
title_sort |
modelling ch 4 emissions from arctic wetlands: effects of hydrological parameterization |
publisher |
Copernicus Publications |
publishDate |
2008 |
url |
https://doaj.org/article/fa842e5d852b405084eecdff6caa6481 |
long_lat |
ENVELOPE(18.829,18.829,68.349,68.349) ENVELOPE(149.609,149.609,70.929,70.929) ENVELOPE(7.337,7.337,62.510,62.510) ENVELOPE(18.861,18.861,68.392,68.392) |
geographic |
Arctic Abisko Indigirka Stordalen Torneträsk |
geographic_facet |
Arctic Abisko Indigirka Stordalen Torneträsk |
genre |
Abisko Arctic Northern Sweden permafrost Siberia |
genre_facet |
Abisko Arctic Northern Sweden permafrost Siberia |
op_source |
Biogeosciences, Vol 5, Iss 1, Pp 111-121 (2008) |
op_relation |
http://www.biogeosciences.net/5/111/2008/bg-5-111-2008.pdf https://doaj.org/toc/1726-4170 https://doaj.org/toc/1726-4189 1726-4170 1726-4189 https://doaj.org/article/fa842e5d852b405084eecdff6caa6481 |
_version_ |
1766140251940585472 |