Global Modeling of the Oceanic Source of Organic Aerosols

The global marine organic aerosol budget is investigated by a 3-dimensional chemistry-transport model considering recently proposed parameterisations of the primary marine organic aerosol (POA) and secondary organic aerosol (SOA) formation from the oxidation of marine volatile organic compounds. MOD...

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Main Authors: Stelios Myriokefalitakis, Elisabetta Vignati, Kostas Tsigaridis, Christos Papadimas, Jean Sciare, Nikolaos Mihalopoulos, Maria Cristina Facchini, Matteo Rinaldi, Frank J. Dentener, Darius Ceburnis, Nikos Hatzianastasiou, Colin D. O'Dowd, Michiel van Weele, Maria Kanakidou
Format: Article
Language:English
Published: Wiley 2010-01-01
Series:Advances in Meteorology
Online Access:http://dx.doi.org/10.1155/2010/939171
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author Stelios Myriokefalitakis
Elisabetta Vignati
Kostas Tsigaridis
Christos Papadimas
Jean Sciare
Nikolaos Mihalopoulos
Maria Cristina Facchini
Matteo Rinaldi
Frank J. Dentener
Darius Ceburnis
Nikos Hatzianastasiou
Colin D. O'Dowd
Michiel van Weele
Maria Kanakidou
author_facet Stelios Myriokefalitakis
Elisabetta Vignati
Kostas Tsigaridis
Christos Papadimas
Jean Sciare
Nikolaos Mihalopoulos
Maria Cristina Facchini
Matteo Rinaldi
Frank J. Dentener
Darius Ceburnis
Nikos Hatzianastasiou
Colin D. O'Dowd
Michiel van Weele
Maria Kanakidou
author_sort Stelios Myriokefalitakis
collection DOAJ
description The global marine organic aerosol budget is investigated by a 3-dimensional chemistry-transport model considering recently proposed parameterisations of the primary marine organic aerosol (POA) and secondary organic aerosol (SOA) formation from the oxidation of marine volatile organic compounds. MODIS and SeaWiFS satellite data of Chlorophyll-a and ECMWF solar incoming radiation, wind speed, and temperature are driving the oceanic emissions in the model. Based on the adopted parameterisations, the SOA and the submicron POA marine sources are evaluated at about 5 Tg yr−1 (∼1.5 Tg C yr−1) and 7 to 8 Tg yr−1 (∼4 Tg C yr−1), respectively. The computed marine SOA originates from the dimethylsulfide oxidation (∼78%), the potentially formed dialkyl amine salts (∼21%), and marine hydrocarbon oxidation (∼0.1%). Comparison of calculations with observations indicates an additional marine source of soluble organic carbon that could be partially encountered by marine POA chemical ageing.
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publishDate 2010-01-01
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series Advances in Meteorology
spelling doaj-art-877c1a7798e4479a842347bfa45ce2b52025-02-03T06:08:01ZengWileyAdvances in Meteorology1687-93091687-93172010-01-01201010.1155/2010/939171939171Global Modeling of the Oceanic Source of Organic AerosolsStelios Myriokefalitakis0Elisabetta Vignati1Kostas Tsigaridis2Christos Papadimas3Jean Sciare4Nikolaos Mihalopoulos5Maria Cristina Facchini6Matteo Rinaldi7Frank J. Dentener8Darius Ceburnis9Nikos Hatzianastasiou10Colin D. O'Dowd11Michiel van Weele12Maria Kanakidou13Environmental Chemical Processes Laboratory, Department of Chemistry, University of Crete, 71003, Heraklion, GreeceInstitute for Environment and Sustainability, European Commission, Joint Research Centre, 21027, Ispra, ItalyNASA Goddard Institute for Space Studies, New York, NY 10025, USADepartment of Physics, University of Ioannina, 54110, Ioannina, GreeceLSCE, CNRS/CEA, 91190, Gif sur Yvette, FranceEnvironmental Chemical Processes Laboratory, Department of Chemistry, University of Crete, 71003, Heraklion, GreeceInstitute of Atmospheric Sciences and Climate, CNR, 40129, Bologna, ItalyInstitute of Atmospheric Sciences and Climate, CNR, 40129, Bologna, ItalyInstitute for Environment and Sustainability, European Commission, Joint Research Centre, 21027, Ispra, ItalySchool of Physics and Environmental Change Institute, National University of Ireland, Galway, IrelandDepartment of Physics, University of Ioannina, 54110, Ioannina, GreeceSchool of Physics and Environmental Change Institute, National University of Ireland, Galway, IrelandRoyal Netherlands Meteorological Institute (KNMI), P.O. Box 201, 3730 AE, De Bilt, The NetherlandsEnvironmental Chemical Processes Laboratory, Department of Chemistry, University of Crete, 71003, Heraklion, GreeceThe global marine organic aerosol budget is investigated by a 3-dimensional chemistry-transport model considering recently proposed parameterisations of the primary marine organic aerosol (POA) and secondary organic aerosol (SOA) formation from the oxidation of marine volatile organic compounds. MODIS and SeaWiFS satellite data of Chlorophyll-a and ECMWF solar incoming radiation, wind speed, and temperature are driving the oceanic emissions in the model. Based on the adopted parameterisations, the SOA and the submicron POA marine sources are evaluated at about 5 Tg yr−1 (∼1.5 Tg C yr−1) and 7 to 8 Tg yr−1 (∼4 Tg C yr−1), respectively. The computed marine SOA originates from the dimethylsulfide oxidation (∼78%), the potentially formed dialkyl amine salts (∼21%), and marine hydrocarbon oxidation (∼0.1%). Comparison of calculations with observations indicates an additional marine source of soluble organic carbon that could be partially encountered by marine POA chemical ageing.http://dx.doi.org/10.1155/2010/939171
spellingShingle Stelios Myriokefalitakis
Elisabetta Vignati
Kostas Tsigaridis
Christos Papadimas
Jean Sciare
Nikolaos Mihalopoulos
Maria Cristina Facchini
Matteo Rinaldi
Frank J. Dentener
Darius Ceburnis
Nikos Hatzianastasiou
Colin D. O'Dowd
Michiel van Weele
Maria Kanakidou
Global Modeling of the Oceanic Source of Organic Aerosols
Advances in Meteorology
title Global Modeling of the Oceanic Source of Organic Aerosols
title_full Global Modeling of the Oceanic Source of Organic Aerosols
title_fullStr Global Modeling of the Oceanic Source of Organic Aerosols
title_full_unstemmed Global Modeling of the Oceanic Source of Organic Aerosols
title_short Global Modeling of the Oceanic Source of Organic Aerosols
title_sort global modeling of the oceanic source of organic aerosols
url http://dx.doi.org/10.1155/2010/939171
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