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Atmospheric observations of Arctic Occean methane emissions up to 82 degrees north
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Permanent Link:
http://dpanther.fiu.edu/dpService/dpPurlService/purl/FI15052541/00001
Material Information
Title:
Atmospheric observations of Arctic Occean methane emissions up to 82 degrees north
Series Title:
Nature Geoscience Magazine Letters
Creator:
E.A. Kort
S.C. Wofsy
B.C. Daube
M. Diao
J.W. Elkins
R.S. Gao
E.J. Hintsa
D.F. Hurst
R. Jimenez
F.L. Moore
J.R. Spackman
M.A. Zondlo
Publisher:
Macmillan Publishers Limited
Publication Date:
2012-04-22
Language:
English
Subjects
Subjects / Keywords:
climate change
Arctic Ocean
methane
greenhouse gases
Notes
Abstract:
Uncertainty in the future atmospheric burden of methane, a potent greenhouse gas1, represents an important challenge to the development of realistic climate projections. The Arctic is home to large reservoirs of methane, in the form of permafrost soils and methane hydrates2, which are vulnerable to destabilization in a warming climate. Furthermore, methane is produced in the surface ocean3 and the surface waters of the Arctic Ocean are supersaturated with respect to methane4,5. However, the fate of this oceanic methane is uncertain. Here, we use airborne observations of methane to assess methane efflux from the remote Arctic Ocean, up to latitudes of 82 [degrees] north. We report layers of increased methane concentrations near the surface ocean, with little or no enhancement in carbon monoxide levels, indicative of a non-combustion source. We further show that high methane concentrations are restricted to areas over open leads and regions with fractional sea-ice cover. Based on the observed gradients in methane concentration, we estimate that sea– air fluxes amount to around 2mgd-1 m-2, comparable to emissions seen on the Siberian shelf. We suggest that the surface waters of the Arctic Ocean represent a potentially important source of methane, which could prove sensitive to changes in sea-ice cover.
Record Information
Source Institution:
Florida International University
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