The response of methane hydrate beneath the seabed offshore Svalbard to ocean warming during the next three centuries
Methane is a potent greenhouse gas and large-scale rapid release of methane from hydrate may have contributed to past abrupt climate change inferred from the geological record. The discovery in 2008 of over 250 plumes of methane gas escaping from the seabed of the West Svalbard continental margin at...
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2013
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ftnerc:oai:nora.nerc.ac.uk:503953 2023-05-15T14:55:08+02:00 The response of methane hydrate beneath the seabed offshore Svalbard to ocean warming during the next three centuries Marin Moreno, Héctor Minshull, Timothy A. Westbrook, Graham K. Sinha, Bablu Sarkar, Sudipta 2013-10-16 text http://nora.nerc.ac.uk/id/eprint/503953/ https://nora.nerc.ac.uk/id/eprint/503953/1/grl50985_MarinMoreno.pdf https://doi.org/10.1002/grl.50985 en eng https://nora.nerc.ac.uk/id/eprint/503953/1/grl50985_MarinMoreno.pdf Marin Moreno, Héctor orcid:0000-0002-3412-1359 Minshull, Timothy A.; Westbrook, Graham K.; Sinha, Bablu; Sarkar, Sudipta. 2013 The response of methane hydrate beneath the seabed offshore Svalbard to ocean warming during the next three centuries. Geophysical Research Letters, 40 (19). 5159-5163. https://doi.org/10.1002/grl.50985 <https://doi.org/10.1002/grl.50985> Publication - Article PeerReviewed 2013 ftnerc https://doi.org/10.1002/grl.50985 2023-02-04T19:38:10Z Methane is a potent greenhouse gas and large-scale rapid release of methane from hydrate may have contributed to past abrupt climate change inferred from the geological record. The discovery in 2008 of over 250 plumes of methane gas escaping from the seabed of the West Svalbard continental margin at ~400 m water depth (mwd) suggests that hydrate is dissociating in the present-day Arctic. Here we model the dynamic response of hydrate-bearing sediments over a period of 2300 years and investigate ocean warming as a possible cause for present-day and likely future dissociation of hydrate, within 350–800 mwd, west of Svalbard. Future temperatures are given by two climate models, HadGEM2 and CCSM4, and scenarios, Representative Concentration Pathways (RCPs) 8.5 and 2.6. Our results suggest that over the next three centuries 5.3–29 Gg yr−1 of methane may be released to the Arctic Ocean on the West Svalbard margin. Article in Journal/Newspaper Arctic Arctic Ocean Climate change Methane hydrate Svalbard Svalbard margin Natural Environment Research Council: NERC Open Research Archive Arctic Arctic Ocean Svalbard Geophysical Research Letters 40 19 5159 5163 |
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Open Polar |
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Natural Environment Research Council: NERC Open Research Archive |
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ftnerc |
language |
English |
description |
Methane is a potent greenhouse gas and large-scale rapid release of methane from hydrate may have contributed to past abrupt climate change inferred from the geological record. The discovery in 2008 of over 250 plumes of methane gas escaping from the seabed of the West Svalbard continental margin at ~400 m water depth (mwd) suggests that hydrate is dissociating in the present-day Arctic. Here we model the dynamic response of hydrate-bearing sediments over a period of 2300 years and investigate ocean warming as a possible cause for present-day and likely future dissociation of hydrate, within 350–800 mwd, west of Svalbard. Future temperatures are given by two climate models, HadGEM2 and CCSM4, and scenarios, Representative Concentration Pathways (RCPs) 8.5 and 2.6. Our results suggest that over the next three centuries 5.3–29 Gg yr−1 of methane may be released to the Arctic Ocean on the West Svalbard margin. |
format |
Article in Journal/Newspaper |
author |
Marin Moreno, Héctor Minshull, Timothy A. Westbrook, Graham K. Sinha, Bablu Sarkar, Sudipta |
spellingShingle |
Marin Moreno, Héctor Minshull, Timothy A. Westbrook, Graham K. Sinha, Bablu Sarkar, Sudipta The response of methane hydrate beneath the seabed offshore Svalbard to ocean warming during the next three centuries |
author_facet |
Marin Moreno, Héctor Minshull, Timothy A. Westbrook, Graham K. Sinha, Bablu Sarkar, Sudipta |
author_sort |
Marin Moreno, Héctor |
title |
The response of methane hydrate beneath the seabed offshore Svalbard to ocean warming during the next three centuries |
title_short |
The response of methane hydrate beneath the seabed offshore Svalbard to ocean warming during the next three centuries |
title_full |
The response of methane hydrate beneath the seabed offshore Svalbard to ocean warming during the next three centuries |
title_fullStr |
The response of methane hydrate beneath the seabed offshore Svalbard to ocean warming during the next three centuries |
title_full_unstemmed |
The response of methane hydrate beneath the seabed offshore Svalbard to ocean warming during the next three centuries |
title_sort |
response of methane hydrate beneath the seabed offshore svalbard to ocean warming during the next three centuries |
publishDate |
2013 |
url |
http://nora.nerc.ac.uk/id/eprint/503953/ https://nora.nerc.ac.uk/id/eprint/503953/1/grl50985_MarinMoreno.pdf https://doi.org/10.1002/grl.50985 |
geographic |
Arctic Arctic Ocean Svalbard |
geographic_facet |
Arctic Arctic Ocean Svalbard |
genre |
Arctic Arctic Ocean Climate change Methane hydrate Svalbard Svalbard margin |
genre_facet |
Arctic Arctic Ocean Climate change Methane hydrate Svalbard Svalbard margin |
op_relation |
https://nora.nerc.ac.uk/id/eprint/503953/1/grl50985_MarinMoreno.pdf Marin Moreno, Héctor orcid:0000-0002-3412-1359 Minshull, Timothy A.; Westbrook, Graham K.; Sinha, Bablu; Sarkar, Sudipta. 2013 The response of methane hydrate beneath the seabed offshore Svalbard to ocean warming during the next three centuries. Geophysical Research Letters, 40 (19). 5159-5163. https://doi.org/10.1002/grl.50985 <https://doi.org/10.1002/grl.50985> |
op_doi |
https://doi.org/10.1002/grl.50985 |
container_title |
Geophysical Research Letters |
container_volume |
40 |
container_issue |
19 |
container_start_page |
5159 |
op_container_end_page |
5163 |
_version_ |
1766326921462808576 |