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dc.contributor.authorAyers, GP
dc.contributor.authorGillett, RW
dc.contributor.authorIvey, JP
dc.contributor.authorSchäfer, B
dc.contributor.authorGabric, A
dc.date.accessioned2019-05-09T00:30:54Z
dc.date.available2019-05-09T00:30:54Z
dc.date.issued1995
dc.identifier.issn0094-8276
dc.identifier.doi10.1029/95GL02484
dc.identifier.urihttp://hdl.handle.net/10072/120097
dc.description.abstractDimethylsulfide (DMS) concentrations measured twice per hour in marine boundary layer air at the Cape Grim baseline station exhibit high variability over timescales as short as several hours. Major sources of this variability are identified as a diurnal cycle associated with the daytime destruction of DMS by reaction with hydroxyl radical, and a strong dependence upon wind speed, with high DMS concentrations at high wind speeds. The wind speed dependence was found to be broadly consistent with the wind speed dependence proposed by Liss and Merlivat [1986] for 10 m wind speed in the range 3.6 to 13 m s−1.
dc.description.peerreviewedYes
dc.languageEnglish
dc.publisherAmerican Geophysical Union
dc.publisher.placeUSA
dc.relation.ispartofpagefrom2513
dc.relation.ispartofpageto2516
dc.relation.ispartofissue18
dc.relation.ispartofjournalGeophysical Research Letters
dc.relation.ispartofvolume22
dc.subject.fieldofresearchEarth Sciences
dc.subject.fieldofresearchcode04
dc.titleShort Term Variability in Marine Atmospheric Dimethylsulphide Concentration
dc.typeJournal article
dc.type.descriptionC1 - Articles
dc.type.codeC - Journal Articles
dc.description.versionPublished
gro.facultyGriffith Sciences, Griffith School of Environment
gro.rights.copyright© 1995 American Geophysical Union. The attached file is reproduced here in accordance with the copyright policy of the publisher. Please refer to the journal's website for access to the definitive, published version.
gro.hasfulltextFull Text
gro.griffith.authorGabric, Albert J.


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