Wind speed dependent size-resolved parameterization for the organic mass fraction of sea spray aerosol

For oceans to be a significant source of primary organic aerosol (POA), sea spray aerosol (SSA) must be highly enriched with organics relative to the bulk seawater. We propose that organic enrichment at the air-sea interface, chemical composition of seawater, and the aerosol size are three main para...

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Main Authors: B. Gantt, N. Meskhidze, M. C. Facchini, M. Rinaldi, D. Ceburnis, C. D. O'Dowd
Format: Article
Language:English
Published: Copernicus Publications 2011-08-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/11/8777/2011/acp-11-8777-2011.pdf
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author B. Gantt
N. Meskhidze
M. C. Facchini
M. Rinaldi
D. Ceburnis
C. D. O'Dowd
author_facet B. Gantt
N. Meskhidze
M. C. Facchini
M. Rinaldi
D. Ceburnis
C. D. O'Dowd
author_sort B. Gantt
collection DOAJ
description For oceans to be a significant source of primary organic aerosol (POA), sea spray aerosol (SSA) must be highly enriched with organics relative to the bulk seawater. We propose that organic enrichment at the air-sea interface, chemical composition of seawater, and the aerosol size are three main parameters controlling the organic mass fraction of sea spray aerosol (OM<sub>SSA</sub>). To test this hypothesis, we developed a new marine POA emission function based on a conceptual relationship between the organic enrichment at the air-sea interface and surface wind speed. The resulting parameterization is explored using aerosol chemical composition and surface wind speed from Atlantic and Pacific coastal stations, and satellite-derived ocean concentrations of chlorophyll-<i>a</i>, dissolved organic carbon, and particulate organic carbon. Of all the parameters examined, a multi-variable logistic regression revealed that the combination of 10 m wind speed and surface chlorophyll-<i>a</i> concentration ([Chl-<i>a</i>]) are the most consistent predictors of OM<sub>SSA</sub>. This relationship, combined with the published aerosol size dependence of OM<sub>SSA</sub>, resulted in a new parameterization for the organic mass fraction of SSA. Global emissions of marine POA are investigated here by applying this newly-developed relationship to existing sea spray emission functions, satellite-derived [Chl-<i>a</i>], and modeled 10 m winds. Analysis of model simulations shows that global annual submicron marine organic emission associated with sea spray is estimated to be from 2.8 to 5.6 Tg C yr<sup>−1</sup>. This study provides additional evidence that marine primary organic aerosols are a globally significant source of organics in the atmosphere.
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spelling doaj.art-450e68b80403412da349b2b0089e4c752022-12-21T19:16:59ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242011-08-0111168777879010.5194/acp-11-8777-2011Wind speed dependent size-resolved parameterization for the organic mass fraction of sea spray aerosolB. GanttN. MeskhidzeM. C. FacchiniM. RinaldiD. CeburnisC. D. O'DowdFor oceans to be a significant source of primary organic aerosol (POA), sea spray aerosol (SSA) must be highly enriched with organics relative to the bulk seawater. We propose that organic enrichment at the air-sea interface, chemical composition of seawater, and the aerosol size are three main parameters controlling the organic mass fraction of sea spray aerosol (OM<sub>SSA</sub>). To test this hypothesis, we developed a new marine POA emission function based on a conceptual relationship between the organic enrichment at the air-sea interface and surface wind speed. The resulting parameterization is explored using aerosol chemical composition and surface wind speed from Atlantic and Pacific coastal stations, and satellite-derived ocean concentrations of chlorophyll-<i>a</i>, dissolved organic carbon, and particulate organic carbon. Of all the parameters examined, a multi-variable logistic regression revealed that the combination of 10 m wind speed and surface chlorophyll-<i>a</i> concentration ([Chl-<i>a</i>]) are the most consistent predictors of OM<sub>SSA</sub>. This relationship, combined with the published aerosol size dependence of OM<sub>SSA</sub>, resulted in a new parameterization for the organic mass fraction of SSA. Global emissions of marine POA are investigated here by applying this newly-developed relationship to existing sea spray emission functions, satellite-derived [Chl-<i>a</i>], and modeled 10 m winds. Analysis of model simulations shows that global annual submicron marine organic emission associated with sea spray is estimated to be from 2.8 to 5.6 Tg C yr<sup>−1</sup>. This study provides additional evidence that marine primary organic aerosols are a globally significant source of organics in the atmosphere.http://www.atmos-chem-phys.net/11/8777/2011/acp-11-8777-2011.pdf
spellingShingle B. Gantt
N. Meskhidze
M. C. Facchini
M. Rinaldi
D. Ceburnis
C. D. O'Dowd
Wind speed dependent size-resolved parameterization for the organic mass fraction of sea spray aerosol
Atmospheric Chemistry and Physics
title Wind speed dependent size-resolved parameterization for the organic mass fraction of sea spray aerosol
title_full Wind speed dependent size-resolved parameterization for the organic mass fraction of sea spray aerosol
title_fullStr Wind speed dependent size-resolved parameterization for the organic mass fraction of sea spray aerosol
title_full_unstemmed Wind speed dependent size-resolved parameterization for the organic mass fraction of sea spray aerosol
title_short Wind speed dependent size-resolved parameterization for the organic mass fraction of sea spray aerosol
title_sort wind speed dependent size resolved parameterization for the organic mass fraction of sea spray aerosol
url http://www.atmos-chem-phys.net/11/8777/2011/acp-11-8777-2011.pdf
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