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dc.contributor.authorGroszko, W.en_US
dc.contributor.authorMoore, RMen_US
dc.date.accessioned2013-06-19T18:02:27Z
dc.date.available2013-06-19T18:02:27Z
dc.date.issued1998-07en_US
dc.identifier.citationGroszko, W., and RM Moore. 1998. "Ocean-atmosphere exchange of methyl bromide: NW Atlantic and Pacific Ocean studies." Journal of Geophysical Research-Atmospheres 103(D13): 16737-16741. DOI:10.1029/98JD00111en_US
dc.identifier.issn2169-897Xen_US
dc.identifier.urihttp://dx.doi.org/10.1029/98JD00111en_US
dc.identifier.urihttp://hdl.handle.net/10222/27146
dc.description.abstractMeasurements of methyl bromide partial pressure and concentration in surface water and air samples in the NW Atlantic Ocean in July 1995 and the Pacific Ocean in October 1995 are presented, Mean atmospheric mixing ratios were found to be 11.4 +/- 0.7 parts per trillion by volume (pptv) for the northern hemisphere and 10.0 +/- 0.5 pptv for the southern hemisphere. Cold, high-latitude water in the Labrador Sea and warm water in the central Pacific were undersaturated in methyl bromide, and some supersaturated waters were found in the Gulf Stream in the Atlantic and around 35 degrees S in the South Pacific. By a simple extrapolation, the global ocean is estimated to be a net sink of 10 (3 to 13) Gg of methyl bromide per year from the atmosphere, with the range including a factor of 2 uncertainty in the piston velocity.en_US
dc.relation.ispartofJournal of Geophysical Research-Atmospheresen_US
dc.titleOcean-atmosphere exchange of methyl bromide: NW Atlantic and Pacific Ocean studiesen_US
dc.typearticleen_US
dc.identifier.volume103en_US
dc.identifier.issue13en_US
dc.identifier.startpage16737en_US
dc.rights.holderThis paper was published by AGU. Copyright 1998 American Geophysical Union
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