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Dichloromethane in North Atlantic waters

dc.contributor.authorMoore, RMen_US
dc.date.accessioned2013-06-19T18:02:25Z
dc.date.available2013-06-19T18:02:25Z
dc.date.issued2004-09en_US
dc.description.abstract[1] Dichloromethane is an atmospheric trace gas that has a tropospheric lifetime on the order of 5 months and has major anthropogenic sources. Evidence has been presented for an oceanic source. This paper reports measurements of dichloromethane in waters of the North Atlantic and Labrador Sea that are interpreted as showing that the compound has a primarily atmospheric source and appears to persist for years to decades in the intermediate and deep ocean. These characteristics have the potential to yield apparent supersaturation of the gas in surface ocean waters which may be incorrectly interpreted as an oceanic source.en_US
dc.identifier.citationMoore, RM. 2004. "Dichloromethane in North Atlantic waters." Journal of Geophysical Research-Oceans 109(C9): 09004-C09004. DOI:10.1029/2004JC002397en_US
dc.identifier.issn0148-0227en_US
dc.identifier.issue9en_US
dc.identifier.startpage09004en_US
dc.identifier.urihttp://dx.doi.org/10.1029/2004JC002397en_US
dc.identifier.urihttp://hdl.handle.net/10222/27119
dc.identifier.volume109en_US
dc.relation.ispartofJournal of Geophysical Research-Oceansen_US
dc.rights.holderThis paper was published by AGU. Copyright 2004 American Geophysical Union
dc.titleDichloromethane in North Atlantic watersen_US
dc.typearticleen_US

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