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dc.contributor.authorOvadnevaite, J.
dc.contributor.authorManders, A.
dc.contributor.authorde Leeuw, G.
dc.contributor.authorCeburnis, D.
dc.contributor.authorMonahan, C.
dc.contributor.authorPartanen, A.-I.
dc.contributor.authorKorhonen, H.
dc.contributor.authorO'Dowd, C. D.
dc.date.accessioned2018-09-20T16:20:54Z
dc.date.available2018-09-20T16:20:54Z
dc.date.issued2014-02-17
dc.identifier.citationOvadnevaite, J. Manders, A.; de Leeuw, G.; Ceburnis, D.; Monahan, C.; Partanen, A.-I.; Korhonen, H.; O'Dowd, C. D. (2014). A sea spray aerosol flux parameterization encapsulating wave state. Atmospheric Chemistry and Physics 14 (4), 1837-1852
dc.identifier.issn1680-7324
dc.identifier.urihttp://hdl.handle.net/10379/13375
dc.description.abstractA new sea spray source function (SSSF), termed Oceanflux Sea Spray Aerosol or OSSA, was derived based on in-situ sea spray aerosol measurements along with meteorological/physical parameters. Submicron sea spray aerosol fluxes derived from particle number concentration measurements at the Mace Head coastal station, on the west coast of Ireland, were used together with open-ocean eddy correlation flux measurements from the Eastern Atlantic Sea Spray, Gas Flux, and Whitecap (SEASAW) project cruise. In the overlapping size range, the data for Mace Head and SEASAW were found to be in a good agreement, which allowed deriving the new SSSF from the combined dataset spanning the dry diameter range from 15 nm to 6 mu m. The OSSA source function has been parameterized in terms of five lognormal modes and the Reynolds number instead of the more commonly used wind speed, thereby encapsulating important influences of wave height, wind history, friction velocity, and viscosity. This formulation accounts for the different flux relationships associated with rising and waning wind speeds since these are included in the Reynolds number. Furthermore, the Reynolds number incorporates the kinematic viscosity of water, thus the SSSF inherently includes dependences on sea surface temperature and salinity. The temperature dependence of the resulting SSSF is similar to that of other in-situ derived source functions and results in lower production fluxes for cold waters and enhanced fluxes from warm waters as compared with SSSF formulations that do not include temperature effects.
dc.publisherCopernicus GmbH
dc.relation.ispartofAtmospheric Chemistry and Physics
dc.rightsAttribution-NonCommercial-NoDerivs 3.0 Ireland
dc.rights.urihttps://creativecommons.org/licenses/by-nc-nd/3.0/ie/
dc.subjectprimary marine aerosol
dc.subjectcloud condensation nuclei
dc.subjectoceanic whitecap coverage
dc.subjectmass-spectrometer
dc.subjectsalt aerosol
dc.subjecterror estimation
dc.subjectboundary-layer
dc.subjectwind-speed
dc.subjectmace head
dc.subjectin-situ
dc.titleA sea spray aerosol flux parameterization encapsulating wave state
dc.typeArticle
dc.identifier.doi10.5194/acp-14-1837-2014
dc.local.publishedsourcehttps://www.atmos-chem-phys.net/14/1837/2014/acp-14-1837-2014.pdf
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Attribution-NonCommercial-NoDerivs 3.0 Ireland
Except where otherwise noted, this item's license is described as Attribution-NonCommercial-NoDerivs 3.0 Ireland