Effects of climate change on methane emissions from seafloor sediments in the Arctic Ocean: A review.

James, Rachael H., Bousquet, Philippe, Bussmann, Ingeborg, Haeckel, Matthias , Kipfer, Rolf, Leifer, Ira, Niemann, Helge, Ostrovsky, Ilia, Piskozub, Jacek, Rehder, Gregor, Treude, Tina , Vielstädte, Lisa and Greinert, Jens (2016) Effects of climate change on methane emissions from seafloor sediments in the Arctic Ocean: A review. Open Access Limnology and Oceanography, 61 (S1). pp. 301-309. DOI 10.1002/lno.10307.

[img]
Preview
Text
James_etal_LnO_2016_Methane-in-the-Arctic.pdf - Published Version
Available under License Creative Commons: Attribution 3.0.

Download (1032Kb) | Preview

Supplementary data:

Abstract

Large quantities of methane are stored in hydrates and permafrost within shallow marine sediments in the Arctic Ocean. These reservoirs are highly sensitive to climate warming, but the fate of methane released from sediments is uncertain. Here, we review the principal physical and biogeochemical processes that regulate methane fluxes across the seabed, the fate of this methane in the water column, and potential for its release to the atmosphere. We find that, at present, fluxes of dissolved methane are significantly moderated by anaerobic and aerobic oxidation of methane. If methane fluxes increase then a greater proportion of methane will be transported
by advection or in the gas phase, which reduces the efficiency of the methanotrophic sink. Higher freshwater discharge to Arctic shelf seas may increase stratification and inhibit transfer of methane gas to surface waters, although there is some evidence that increased stratification may lead to warming of sub-pycnocline waters, increasing the potential for hydrate dissociation. Loss of sea-ice is likely to increase wind speeds and seaair
exchange of methane will consequently increase. Studies of the distribution and cycling of methane beneath and within sea ice are limited, but it seems likely that the sea-air methane flux is higher during melting in seasonally
ice-covered regions. Our review reveals that increased observations around especially the anaerobic and aerobic oxidation of methane, bubble transport, and the effects of ice cover, are required to fully understand the linkages and feedback pathways between climate warming and release of methane from marine sediments.

Document Type: Article
Funder compliance: info:eu-repo/grantAgreement/EC/FP7/603418
Additional Information: In: Special Issue: Methane Emissions from Oceans, Wetlands, and Freshwater Habitats: New Perspectives and Feedbacks on Climate. Edited by: Kimberly Wickland and Leila Hamdan. - WOS:000388560900021
Keywords: Methane, Arctic, gas fluxes, global impact
Research affiliation: NOC
OceanRep > GEOMAR > FB2 Marine Biogeochemistry > FB2-MG Marine Geosystems
OceanRep > GEOMAR > FB2 Marine Biogeochemistry > FB2-MG Marine Geosystems > DeepSea Monitoring
AWI
Kiel University
Refereed: Yes
Open Access Journal?: No
DOI etc.: 10.1002/lno.10307
ISSN: 0024-3590
Projects: COST, PERGAMON, MIDAS, OceanFlux Greenhouse Gases Evolution, Growing of Arctic Ecosystem
Contribution Number:
ProjectNumber
DSM18
Date Deposited: 20 May 2016 07:28
Last Modified: 19 Jul 2019 09:19
URI: http://oceanrep.geomar.de/id/eprint/32895

Actions (login required)

View Item View Item

Document Downloads

More statistics for this item...