Methane emission bursts from permafrost environments during autumn freeze-in: New insights from ground-penetrating radar
Large amounts of methane (CH4) are known to be emitted from permafrost environments during the autumn freeze-in, but the specific soil conditions leading up to these bursts are unclear. Therefore, we used an ultrawide band ground-penetrating radar in Northeast Greenland in autumn 2009 to estimate th...
Published in: | Geophysical Research Letters |
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American Geophysical Union (AGU)
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Online Access: | https://lup.lub.lu.se/record/7766980 https://doi.org/10.1002/2015GL065034 |
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ftulundlup:oai:lup.lub.lu.se:4fd1574e-df01-434e-876b-9d94478459ad 2023-05-15T16:27:27+02:00 Methane emission bursts from permafrost environments during autumn freeze-in: New insights from ground-penetrating radar Pirk, Norbert Santos, Telmo Gustafson, Carl Johansson, Anders J Tufvesson, Fredrik Parmentier, Frans-Jan Mastepanov, Mikhail Christensen, Torben 2015 https://lup.lub.lu.se/record/7766980 https://doi.org/10.1002/2015GL065034 eng eng American Geophysical Union (AGU) https://lup.lub.lu.se/record/7766980 http://dx.doi.org/10.1002/2015GL065034 wos:000363410800026 scopus:84941734654 Geophysical Research Letters; 42(16), pp 6732-6738 (2015) ISSN: 1944-8007 Geosciences Multidisciplinary Electrical Engineering Electronic Engineering Information Engineering ground-penetrating radar Greenland autumn freeze-in methane frequency domain contributiontojournal/article info:eu-repo/semantics/article text 2015 ftulundlup https://doi.org/10.1002/2015GL065034 2023-02-01T23:29:09Z Large amounts of methane (CH4) are known to be emitted from permafrost environments during the autumn freeze-in, but the specific soil conditions leading up to these bursts are unclear. Therefore, we used an ultrawide band ground-penetrating radar in Northeast Greenland in autumn 2009 to estimate the volumetric composition inside the soil through dielectric characterization from 200 to 3200 MHz. Our results suggest a compression of the gas reservoir during the phase transition of soil water, which is accompanied by a peak in surface CH4 emissions. About 1 week thereafter, there seems to be a decompression event, consistent with ground cracking which allows the gas reservoir to expand again. This coincides with the largest CH4 emission, exceeding the summer maximum by a factor of 4. We argue that these complementary measurement techniques are needed to come to an understanding of tundra CH4 bursts connected to soil freezing. Article in Journal/Newspaper Greenland permafrost Tundra Lund University Publications (LUP) Greenland Geophysical Research Letters 42 16 6732 6738 |
institution |
Open Polar |
collection |
Lund University Publications (LUP) |
op_collection_id |
ftulundlup |
language |
English |
topic |
Geosciences Multidisciplinary Electrical Engineering Electronic Engineering Information Engineering ground-penetrating radar Greenland autumn freeze-in methane frequency domain |
spellingShingle |
Geosciences Multidisciplinary Electrical Engineering Electronic Engineering Information Engineering ground-penetrating radar Greenland autumn freeze-in methane frequency domain Pirk, Norbert Santos, Telmo Gustafson, Carl Johansson, Anders J Tufvesson, Fredrik Parmentier, Frans-Jan Mastepanov, Mikhail Christensen, Torben Methane emission bursts from permafrost environments during autumn freeze-in: New insights from ground-penetrating radar |
topic_facet |
Geosciences Multidisciplinary Electrical Engineering Electronic Engineering Information Engineering ground-penetrating radar Greenland autumn freeze-in methane frequency domain |
description |
Large amounts of methane (CH4) are known to be emitted from permafrost environments during the autumn freeze-in, but the specific soil conditions leading up to these bursts are unclear. Therefore, we used an ultrawide band ground-penetrating radar in Northeast Greenland in autumn 2009 to estimate the volumetric composition inside the soil through dielectric characterization from 200 to 3200 MHz. Our results suggest a compression of the gas reservoir during the phase transition of soil water, which is accompanied by a peak in surface CH4 emissions. About 1 week thereafter, there seems to be a decompression event, consistent with ground cracking which allows the gas reservoir to expand again. This coincides with the largest CH4 emission, exceeding the summer maximum by a factor of 4. We argue that these complementary measurement techniques are needed to come to an understanding of tundra CH4 bursts connected to soil freezing. |
format |
Article in Journal/Newspaper |
author |
Pirk, Norbert Santos, Telmo Gustafson, Carl Johansson, Anders J Tufvesson, Fredrik Parmentier, Frans-Jan Mastepanov, Mikhail Christensen, Torben |
author_facet |
Pirk, Norbert Santos, Telmo Gustafson, Carl Johansson, Anders J Tufvesson, Fredrik Parmentier, Frans-Jan Mastepanov, Mikhail Christensen, Torben |
author_sort |
Pirk, Norbert |
title |
Methane emission bursts from permafrost environments during autumn freeze-in: New insights from ground-penetrating radar |
title_short |
Methane emission bursts from permafrost environments during autumn freeze-in: New insights from ground-penetrating radar |
title_full |
Methane emission bursts from permafrost environments during autumn freeze-in: New insights from ground-penetrating radar |
title_fullStr |
Methane emission bursts from permafrost environments during autumn freeze-in: New insights from ground-penetrating radar |
title_full_unstemmed |
Methane emission bursts from permafrost environments during autumn freeze-in: New insights from ground-penetrating radar |
title_sort |
methane emission bursts from permafrost environments during autumn freeze-in: new insights from ground-penetrating radar |
publisher |
American Geophysical Union (AGU) |
publishDate |
2015 |
url |
https://lup.lub.lu.se/record/7766980 https://doi.org/10.1002/2015GL065034 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Greenland permafrost Tundra |
genre_facet |
Greenland permafrost Tundra |
op_source |
Geophysical Research Letters; 42(16), pp 6732-6738 (2015) ISSN: 1944-8007 |
op_relation |
https://lup.lub.lu.se/record/7766980 http://dx.doi.org/10.1002/2015GL065034 wos:000363410800026 scopus:84941734654 |
op_doi |
https://doi.org/10.1002/2015GL065034 |
container_title |
Geophysical Research Letters |
container_volume |
42 |
container_issue |
16 |
container_start_page |
6732 |
op_container_end_page |
6738 |
_version_ |
1766016620912705536 |