Environmental controls on ecosystem-scale CH4 emission from polygonal tundra in the Lena River Delta, Siberia

We present the first ecosystem-scale methane flux data from a northern Siberian tundra ecosystem covering the entire snow-free period from spring thaw until initial freeze-back. Eddy covariance measurements of methane emission were carried out from the beginning of June until the end of September in...

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Published in:Journal of Geophysical Research
Main Authors: Sachs, T., Wille, C., Boike, J., Kutzbach, L.
Format: Article in Journal/Newspaper
Language:English
Published: 2008
Subjects:
Online Access:http://hdl.handle.net/11858/00-001M-0000-0018-2DAA-4
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spelling ftpubman:oai:pure.mpg.de:item_1920957 2023-08-20T04:04:49+02:00 Environmental controls on ecosystem-scale CH4 emission from polygonal tundra in the Lena River Delta, Siberia Sachs, T. Wille, C. Boike, J. Kutzbach, L. 2008 http://hdl.handle.net/11858/00-001M-0000-0018-2DAA-4 eng eng info:eu-repo/semantics/altIdentifier/doi/10.1029/2007JG000505 http://hdl.handle.net/11858/00-001M-0000-0018-2DAA-4 Journal of Geophysical Research-Biogeosciences info:eu-repo/semantics/article 2008 ftpubman https://doi.org/10.1029/2007JG000505 2023-08-01T22:01:36Z We present the first ecosystem-scale methane flux data from a northern Siberian tundra ecosystem covering the entire snow-free period from spring thaw until initial freeze-back. Eddy covariance measurements of methane emission were carried out from the beginning of June until the end of September in the southern central part of the Lena River Delta (72 degrees 22'N, 126 degrees 30'E). The study site is located in the zone of continuous permafrost and is characterized by Arctic continental climate with very low precipitation and a mean annual temperature of -14.7 degrees C. We found relatively low fluxes of on average 18.7 mg m(-2) d(-1), which we consider to be because of (1) extremely cold permafrost, (2) substrate limitation of the methanogenic archaea, and (3) a relatively high surface coverage of noninundated, moderately moist areas. Near-surface turbulence as measured by the eddy covariance system in 4 m above the ground surface was identified as the most important control on ecosystem-scale methane emission and explained about 60% of the variance in emissions, while soil temperature explained only 8%. In addition, atmospheric pressure was found to significantly improve an exponential model based on turbulence and soil temperature. Ebullition from waterlogged areas triggered by decreasing atmospheric pressure and near-surface turbulence is thought to be an important pathway that warrants more attention in future studies. The close coupling of methane fluxes and atmospheric parameters demonstrated here raises questions regarding the reliability of enclosure-based measurements, which inherently exclude these parameters. Article in Journal/Newspaper Arctic lena river permafrost Tundra Siberia Max Planck Society: MPG.PuRe Arctic Journal of Geophysical Research 113
institution Open Polar
collection Max Planck Society: MPG.PuRe
op_collection_id ftpubman
language English
description We present the first ecosystem-scale methane flux data from a northern Siberian tundra ecosystem covering the entire snow-free period from spring thaw until initial freeze-back. Eddy covariance measurements of methane emission were carried out from the beginning of June until the end of September in the southern central part of the Lena River Delta (72 degrees 22'N, 126 degrees 30'E). The study site is located in the zone of continuous permafrost and is characterized by Arctic continental climate with very low precipitation and a mean annual temperature of -14.7 degrees C. We found relatively low fluxes of on average 18.7 mg m(-2) d(-1), which we consider to be because of (1) extremely cold permafrost, (2) substrate limitation of the methanogenic archaea, and (3) a relatively high surface coverage of noninundated, moderately moist areas. Near-surface turbulence as measured by the eddy covariance system in 4 m above the ground surface was identified as the most important control on ecosystem-scale methane emission and explained about 60% of the variance in emissions, while soil temperature explained only 8%. In addition, atmospheric pressure was found to significantly improve an exponential model based on turbulence and soil temperature. Ebullition from waterlogged areas triggered by decreasing atmospheric pressure and near-surface turbulence is thought to be an important pathway that warrants more attention in future studies. The close coupling of methane fluxes and atmospheric parameters demonstrated here raises questions regarding the reliability of enclosure-based measurements, which inherently exclude these parameters.
format Article in Journal/Newspaper
author Sachs, T.
Wille, C.
Boike, J.
Kutzbach, L.
spellingShingle Sachs, T.
Wille, C.
Boike, J.
Kutzbach, L.
Environmental controls on ecosystem-scale CH4 emission from polygonal tundra in the Lena River Delta, Siberia
author_facet Sachs, T.
Wille, C.
Boike, J.
Kutzbach, L.
author_sort Sachs, T.
title Environmental controls on ecosystem-scale CH4 emission from polygonal tundra in the Lena River Delta, Siberia
title_short Environmental controls on ecosystem-scale CH4 emission from polygonal tundra in the Lena River Delta, Siberia
title_full Environmental controls on ecosystem-scale CH4 emission from polygonal tundra in the Lena River Delta, Siberia
title_fullStr Environmental controls on ecosystem-scale CH4 emission from polygonal tundra in the Lena River Delta, Siberia
title_full_unstemmed Environmental controls on ecosystem-scale CH4 emission from polygonal tundra in the Lena River Delta, Siberia
title_sort environmental controls on ecosystem-scale ch4 emission from polygonal tundra in the lena river delta, siberia
publishDate 2008
url http://hdl.handle.net/11858/00-001M-0000-0018-2DAA-4
geographic Arctic
geographic_facet Arctic
genre Arctic
lena river
permafrost
Tundra
Siberia
genre_facet Arctic
lena river
permafrost
Tundra
Siberia
op_source Journal of Geophysical Research-Biogeosciences
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1029/2007JG000505
http://hdl.handle.net/11858/00-001M-0000-0018-2DAA-4
op_doi https://doi.org/10.1029/2007JG000505
container_title Journal of Geophysical Research
container_volume 113
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