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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Format: | Article |
Language: | English |
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Wiley
2010-01-01
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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. |
format | Article |
id | doaj-art-877c1a7798e4479a842347bfa45ce2b5 |
institution | Kabale University |
issn | 1687-9309 1687-9317 |
language | English |
publishDate | 2010-01-01 |
publisher | Wiley |
record_format | Article |
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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