Effect of wind speed on aerosol optical depth over remote oceans, based on data from the Maritime Aerosol Network

dc.bibliographicCitation.firstPage377eng
dc.bibliographicCitation.issue2eng
dc.bibliographicCitation.lastPage388eng
dc.bibliographicCitation.volume5
dc.contributor.authorSmirnov, A.
dc.contributor.authorSayer, A.M.
dc.contributor.authorHolben, B.N.
dc.contributor.authorHsu, N.C.
dc.contributor.authorSakerin, S.M.
dc.contributor.authorMacke, A.
dc.contributor.authorNelson, N.B.
dc.contributor.authorCourcoux, Y.
dc.contributor.authorSmyth, T.J.
dc.contributor.authorCroot, P.
dc.contributor.authorQuinn, P.K.
dc.contributor.authorSciare, J.
dc.contributor.authorGulev, S.K.
dc.contributor.authorPiketh, S.
dc.contributor.authorLosno, R.
dc.contributor.authorKinne, S.
dc.contributor.authorRadionov, V.F.
dc.date.accessioned2018-01-05T11:15:08Z
dc.date.available2019-06-26T17:20:49Z
dc.date.issued2012
dc.description.abstractThe Maritime Aerosol Network (MAN) has been collecting data over the oceans since November 2006. The MAN archive provides a valuable resource for aerosol studies in maritime environments. In the current paper we investigate correlations between ship-borne aerosol optical depth (AOD) and near-surface wind speed, either measured (onboard or from satellite) or modeled (NCEP). According to our analysis, wind speed influences columnar aerosol optical depth, although the slope of the linear regression between AOD and wind speed is not steep (~0.004–0.005), even for strong winds over 10 m s−1. The relationships show significant scatter (correlation coefficients typically in the range 0.3–0.5); the majority of this scatter can be explained by the uncertainty on the input data. The various wind speed sources considered yield similar patterns. Results are in good agreement with the majority of previously published relationships between surface wind speed and ship-based or satellite-based AOD measurements. The basic relationships are similar for all the wind speed sources considered; however, the gradient of the relationship varies by around a factor of two depending on the wind data used.eng
dc.description.versionpublishedVersioneng
dc.formatapplication/pdf
dc.identifier.urihttps://doi.org/10.34657/906
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/806
dc.language.isoengeng
dc.publisherMünchen : European Geopyhsical Unioneng
dc.relation.doihttps://doi.org/10.5194/amt-5-377-2012
dc.relation.ispartofseriesAtmospheric Measurement Techniques, Volume 5, Issue 2, Page 377-388eng
dc.rights.licenseCC BY 3.0 Unportedeng
dc.rights.urihttps://creativecommons.org/licenses/by/3.0/eng
dc.subjectaerosoleng
dc.subjectmaritime transportationeng
dc.subjectoptical deptheng
dc.subjectsatellite dataeng
dc.subjectshipborne measurementeng
dc.subjectwind velocityeng
dc.subject.ddc550eng
dc.titleEffect of wind speed on aerosol optical depth over remote oceans, based on data from the Maritime Aerosol Networkeng
dc.typearticleeng
dc.typeTexteng
dcterms.bibliographicCitation.journalTitleAtmospheric Measurement Techniqueseng
tib.accessRightsopenAccesseng
wgl.contributorTROPOSeng
wgl.subjectGeowissenschafteneng
wgl.typeZeitschriftenartikeleng
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