Articles | Volume 14, issue 11
https://doi.org/10.5194/tc-14-3829-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-14-3829-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
09 Nov 2020
Research article |
| 09 Nov 2020
| 09 Nov 2020
Sub-permafrost methane seepage from open-system pingos in Svalbard
Andrew J. Hodson
CORRESPONDING AUTHOR
Department of Arctic Geology, University Centre in Svalbard (UNIS),
9171 Longyearbyen, Norway
Department of Environmental Science, Western Norway University of
Applied Sciences, Røyrgata 6, 6856 Sogndal, Norway
Aga Nowak
Department of Arctic Geology, University Centre in Svalbard (UNIS),
9171 Longyearbyen, Norway
Mikkel T. Hornum
Department of Arctic Geology, University Centre in Svalbard (UNIS),
9171 Longyearbyen, Norway
Department of Geosciences and Natural Resource Management, University
of Copenhagen, 1350 Copenhagen K, Copenhagen, Denmark
Kim Senger
Department of Arctic Geology, University Centre in Svalbard (UNIS),
9171 Longyearbyen, Norway
Kelly Redeker
Department of Biology, University of York, York, YO10 5DD, UK
Hanne H. Christiansen
Department of Arctic Geology, University Centre in Svalbard (UNIS),
9171 Longyearbyen, Norway
Søren Jessen
Department of Geosciences and Natural Resource Management, University
of Copenhagen, 1350 Copenhagen K, Copenhagen, Denmark
Peter Betlem
Department of Arctic Geology, University Centre in Svalbard (UNIS),
9171 Longyearbyen, Norway
Steve F. Thornton
Department of Civil and Structural Engineering, University of
Sheffield, Sheffield, S10 2TN, UK
Alexandra V. Turchyn
Department of Earth Sciences, University of Cambridge, Cambridge, CB2 3EQ, UK
Snorre Olaussen
Department of Arctic Geology, University Centre in Svalbard (UNIS),
9171 Longyearbyen, Norway
Alina Marca
School of Environmental Sciences, University of East Anglia, Norwich,
NR4 7TJ, UK
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Cited
22 citations as recorded by crossref.
- Active gas seepage in western Spitsbergen fjords, Svalbard archipelago: spatial extent and geological controls N. Rodes et al. 10.3389/feart.2023.1173477
- An overview of sedimentary volcanism on Mars P. Brož et al. 10.5194/esurf-11-633-2023
- Seismic and Electrical Geophysical Characterization of an Incipient Coastal Open‐System Pingo: Lagoon Pingo, Svalbard C. Hammock et al. 10.1029/2021EA002093
- Trajectories of freshwater microbial genomics and greenhouse gas saturation upon glacial retreat J. Wei et al. 10.1038/s41467-023-38806-w
- Numerical modelling of permafrost spring discharge and open-system pingo formation induced by basal permafrost aggradation M. Hornum et al. 10.5194/tc-14-4627-2020
- Extensive glacitectonism and rapid deglacial fluid expulsion in the northeastern Barents Sea A. Montelli et al. 10.1038/s43247-024-01512-6
- The importance of topographic gradients in alpine permafrost modeling J. Beddrich et al. 10.1016/j.advwatres.2022.104321
- Permafrost saline water and Early to mid-Holocene permafrost aggradation in Svalbard D. Rotem et al. 10.5194/tc-17-3363-2023
- Ra isotope perspective on the hydrology and continuity of permafrost in the high Arctic D. Rotem et al. 10.1016/j.scitotenv.2024.175412
- Targeting methanotrophs and isolation of a novel psychrophilic Methylobacter species from a terrestrial Arctic alkaline methane seep in Lagoon Pingo, Central Spitsbergen (78° N) S. Patil et al. 10.1007/s10482-024-01953-1
- Svalbard Composite Tectono-Sedimentary Element, Barents Sea S. Olaussen et al. 10.1144/M57-2021-36
- Effects of glacier retreat upon glacier-groundwater coupling and biogeochemistry in Central Svalbard A. Hodson et al. 10.1016/j.jhydrol.2023.129894
- Pingo drilling reveals sodium–chloride‐dominated massive ice in Grøndalen, Spitsbergen V. Demidov et al. 10.1002/ppp.2124
- Arctic Spring Systems Driven by Permafrost Aggradation M. Hornum et al. 10.1029/2023GL104719
- Thaw slump development and other rapid permafrost disturbances in Hollendardalen Valley, Svalbard V. Demidov et al. 10.1016/j.polar.2024.101122
- Distribution of pingos on Svalbard V. Demidov et al. 10.1016/j.geomorph.2022.108326
- Groundwater Flow Through Continuous Permafrost Along Geological Boundary Revealed by Electrical Resistivity Tomography M. Hornum et al. 10.1029/2021GL092757
- Permafrost and groundwater interaction: current state and future perspective M. Diak et al. 10.3389/feart.2023.1254309
- Groundwater springs formed during glacial retreat are a large source of methane in the high Arctic G. Kleber et al. 10.1038/s41561-023-01210-6
- Characterization of atmospheric methane release in the outer Mackenzie River delta from biogenic and thermogenic sources D. Wesley et al. 10.5194/tc-17-5283-2023
- A Review on Geological View of Svalbard with its Infrastructure and Strategies Ş. Yalçınkaya et al. 10.30897/ijegeo.1081659
- Geocryological and Hydrogeological Conditions of the Western Part of Nordenskiold Land (Spitsbergen Archipelago) N. Demidov et al. 10.1134/S000143382011002X
20 citations as recorded by crossref.
- Active gas seepage in western Spitsbergen fjords, Svalbard archipelago: spatial extent and geological controls N. Rodes et al. 10.3389/feart.2023.1173477
- An overview of sedimentary volcanism on Mars P. Brož et al. 10.5194/esurf-11-633-2023
- Seismic and Electrical Geophysical Characterization of an Incipient Coastal Open‐System Pingo: Lagoon Pingo, Svalbard C. Hammock et al. 10.1029/2021EA002093
- Trajectories of freshwater microbial genomics and greenhouse gas saturation upon glacial retreat J. Wei et al. 10.1038/s41467-023-38806-w
- Numerical modelling of permafrost spring discharge and open-system pingo formation induced by basal permafrost aggradation M. Hornum et al. 10.5194/tc-14-4627-2020
- Extensive glacitectonism and rapid deglacial fluid expulsion in the northeastern Barents Sea A. Montelli et al. 10.1038/s43247-024-01512-6
- The importance of topographic gradients in alpine permafrost modeling J. Beddrich et al. 10.1016/j.advwatres.2022.104321
- Permafrost saline water and Early to mid-Holocene permafrost aggradation in Svalbard D. Rotem et al. 10.5194/tc-17-3363-2023
- Ra isotope perspective on the hydrology and continuity of permafrost in the high Arctic D. Rotem et al. 10.1016/j.scitotenv.2024.175412
- Targeting methanotrophs and isolation of a novel psychrophilic Methylobacter species from a terrestrial Arctic alkaline methane seep in Lagoon Pingo, Central Spitsbergen (78° N) S. Patil et al. 10.1007/s10482-024-01953-1
- Svalbard Composite Tectono-Sedimentary Element, Barents Sea S. Olaussen et al. 10.1144/M57-2021-36
- Effects of glacier retreat upon glacier-groundwater coupling and biogeochemistry in Central Svalbard A. Hodson et al. 10.1016/j.jhydrol.2023.129894
- Pingo drilling reveals sodium–chloride‐dominated massive ice in Grøndalen, Spitsbergen V. Demidov et al. 10.1002/ppp.2124
- Arctic Spring Systems Driven by Permafrost Aggradation M. Hornum et al. 10.1029/2023GL104719
- Thaw slump development and other rapid permafrost disturbances in Hollendardalen Valley, Svalbard V. Demidov et al. 10.1016/j.polar.2024.101122
- Distribution of pingos on Svalbard V. Demidov et al. 10.1016/j.geomorph.2022.108326
- Groundwater Flow Through Continuous Permafrost Along Geological Boundary Revealed by Electrical Resistivity Tomography M. Hornum et al. 10.1029/2021GL092757
- Permafrost and groundwater interaction: current state and future perspective M. Diak et al. 10.3389/feart.2023.1254309
- Groundwater springs formed during glacial retreat are a large source of methane in the high Arctic G. Kleber et al. 10.1038/s41561-023-01210-6
- Characterization of atmospheric methane release in the outer Mackenzie River delta from biogenic and thermogenic sources D. Wesley et al. 10.5194/tc-17-5283-2023
2 citations as recorded by crossref.
Latest update: 13 Dec 2024
Short summary
Methane stored below permafrost is an unknown quantity in the Arctic greenhouse gas budget. In coastal areas with rising sea levels, much of the methane seeps into the sea and is removed before it reaches the atmosphere. However, where land uplift outpaces rising sea levels, the former seabed freezes, pressurising methane-rich groundwater beneath, which then escapes via permafrost seepages called pingos. We describe this mechanism and the origins of the methane discharging from Svalbard pingos.
Methane stored below permafrost is an unknown quantity in the Arctic greenhouse gas budget. In...
