Replication Data for: Reduced methane seepage from Arctic sediments during cold bottom-water conditions

This dataset contains all the necessary data for reproducing the results in the article. "Reduced methane seepage from Arctic sediments during cold bottom-water conditions" Abstract: Large amounts of methane are trapped within sub-seabed sediments in the Arctic ocean. Seasonal bottom water...

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Main Authors: Ferré, Bénédicte, Jansson, Pär, Moser, Manuel, Serov, Pavel, Portnov, Alexei, Graves, Carolyn, Panieri, Giuliana, Gründger, Friederike, Berndt, Christian, Lehmann, Moritz F, Niemann, Helge
Format: Other/Unknown Material
Language:English
Published: DataverseNO 2016
Subjects:
Online Access:https://doi.org/10.18710/EIFZ2J
id ftdataverseno:doi:10.18710/EIFZ2J
record_format openpolar
spelling ftdataverseno:doi:10.18710/EIFZ2J 2023-10-29T02:33:27+01:00 Replication Data for: Reduced methane seepage from Arctic sediments during cold bottom-water conditions Ferré, Bénédicte Jansson, Pär Moser, Manuel Serov, Pavel Portnov, Alexei Graves, Carolyn Panieri, Giuliana Gründger, Friederike Berndt, Christian Lehmann, Moritz F Niemann, Helge Jansson, Pär 2016-05-08 https://doi.org/10.18710/EIFZ2J English eng DataverseNO https://doi.org/10.18710/EIFZ2J Earth and Environmental Sciences Methane Cold seep Variability Arctic Microbial oxidation Flare Backscatter Ocean Seasonal Water temperature Salinity Pressure/ Depth Methane free gas flow rate Methane concentration Methane oxidation rates 2016 ftdataverseno https://doi.org/10.18710/EIFZ2J 2023-10-04T22:53:37Z This dataset contains all the necessary data for reproducing the results in the article. "Reduced methane seepage from Arctic sediments during cold bottom-water conditions" Abstract: Large amounts of methane are trapped within sub-seabed sediments in the Arctic ocean. Seasonal bottom water warming may induce the release of methane from the seafloor, yet methane seepage surveys mainly occur in summer. Here, we compare the seepage activity along the gas hydrate stability limit offshore Svalbard between cold and warm seasons. Hydro-acoustic surveys revealed decreased seepage activity during cold bottom water conditions, with 43 % fewer flares and methane release rates than under warmer conditions. For the first time, we demonstrate that cold seeps “hibernate” during cold seasons when more free methane gas becomes trapped in the sub-seabed sediments. Such a greenhouse gas capacitor increases the potential for methane release during summer months. Seasonal bottom water temperature variations are common in the Arctic continental shelves, and thus methane-seep hibernation is likely a widespread phenomenon underappreciated in previous global methane budgets. Other/Unknown Material Arctic Arctic Ocean Svalbard DataverseNO
institution Open Polar
collection DataverseNO
op_collection_id ftdataverseno
language English
topic Earth and Environmental Sciences
Methane
Cold seep
Variability
Arctic
Microbial oxidation
Flare
Backscatter
Ocean
Seasonal
spellingShingle Earth and Environmental Sciences
Methane
Cold seep
Variability
Arctic
Microbial oxidation
Flare
Backscatter
Ocean
Seasonal
Ferré, Bénédicte
Jansson, Pär
Moser, Manuel
Serov, Pavel
Portnov, Alexei
Graves, Carolyn
Panieri, Giuliana
Gründger, Friederike
Berndt, Christian
Lehmann, Moritz F
Niemann, Helge
Replication Data for: Reduced methane seepage from Arctic sediments during cold bottom-water conditions
topic_facet Earth and Environmental Sciences
Methane
Cold seep
Variability
Arctic
Microbial oxidation
Flare
Backscatter
Ocean
Seasonal
description This dataset contains all the necessary data for reproducing the results in the article. "Reduced methane seepage from Arctic sediments during cold bottom-water conditions" Abstract: Large amounts of methane are trapped within sub-seabed sediments in the Arctic ocean. Seasonal bottom water warming may induce the release of methane from the seafloor, yet methane seepage surveys mainly occur in summer. Here, we compare the seepage activity along the gas hydrate stability limit offshore Svalbard between cold and warm seasons. Hydro-acoustic surveys revealed decreased seepage activity during cold bottom water conditions, with 43 % fewer flares and methane release rates than under warmer conditions. For the first time, we demonstrate that cold seeps “hibernate” during cold seasons when more free methane gas becomes trapped in the sub-seabed sediments. Such a greenhouse gas capacitor increases the potential for methane release during summer months. Seasonal bottom water temperature variations are common in the Arctic continental shelves, and thus methane-seep hibernation is likely a widespread phenomenon underappreciated in previous global methane budgets.
author2 Jansson, Pär
format Other/Unknown Material
author Ferré, Bénédicte
Jansson, Pär
Moser, Manuel
Serov, Pavel
Portnov, Alexei
Graves, Carolyn
Panieri, Giuliana
Gründger, Friederike
Berndt, Christian
Lehmann, Moritz F
Niemann, Helge
author_facet Ferré, Bénédicte
Jansson, Pär
Moser, Manuel
Serov, Pavel
Portnov, Alexei
Graves, Carolyn
Panieri, Giuliana
Gründger, Friederike
Berndt, Christian
Lehmann, Moritz F
Niemann, Helge
author_sort Ferré, Bénédicte
title Replication Data for: Reduced methane seepage from Arctic sediments during cold bottom-water conditions
title_short Replication Data for: Reduced methane seepage from Arctic sediments during cold bottom-water conditions
title_full Replication Data for: Reduced methane seepage from Arctic sediments during cold bottom-water conditions
title_fullStr Replication Data for: Reduced methane seepage from Arctic sediments during cold bottom-water conditions
title_full_unstemmed Replication Data for: Reduced methane seepage from Arctic sediments during cold bottom-water conditions
title_sort replication data for: reduced methane seepage from arctic sediments during cold bottom-water conditions
publisher DataverseNO
publishDate 2016
url https://doi.org/10.18710/EIFZ2J
genre Arctic
Arctic Ocean
Svalbard
genre_facet Arctic
Arctic Ocean
Svalbard
op_relation https://doi.org/10.18710/EIFZ2J
op_doi https://doi.org/10.18710/EIFZ2J
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