Variability of sub-micrometer particle number size distributions and concentrations in the Western Mediterranean regional background
This study focuses on the daily and seasonal variability of particle number size distributions and concentrations, performed at the Montseny (MSY) regional background station in the western Mediterranean from October 2010 to June 2011. Particle number concentrations at MSY were shown to be within ra...
| Autores: | , , , , , |
|---|---|
| Tipo de recurso: | artículo |
| Estado: | Versión aceptada para publicación |
| Fecha de publicación: | 2013 |
| País: | España |
| Institución: | Consejo Superior de Investigaciones Científicas (CSIC) |
| Repositorio: | DIGITAL.CSIC. Repositorio Institucional del CSIC |
| OAI Identifier: | oai:digital.csic.es:10261/122751 |
| Acceso en línea: | http://hdl.handle.net/10261/122751 |
| Access Level: | acceso abierto |
| Palabra clave: | Nucleation Number concentration Photochemistry Western Mediterranean Sub-micrometer particle size distribution |
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Variability of sub-micrometer particle number size distributions and concentrations in the Western Mediterranean regional backgroundCusack, MichaelPérez, NoemíPey, JorgeWiedensohler, AlfredAlastuey, AndrésQuerol, XavierNucleationNumber concentrationPhotochemistryWestern MediterraneanSub-micrometer particle size distributionThis study focuses on the daily and seasonal variability of particle number size distributions and concentrations, performed at the Montseny (MSY) regional background station in the western Mediterranean from October 2010 to June 2011. Particle number concentrations at MSY were shown to be within range of various other sites across Europe reported in literature, but the seasonality of the particle number size distributions revealed significant differences. The Aitken mode is the dominant particle mode at MSY, with arithmetic mean concentrations of 1698 cm3, followed by the accumulation mode (877 cm-3) and the nucleation mode (246 cm-3). Concentrations showed a strong seasonal variability with large increases in particle number concentrations observed from the colder to warmer months. The modality of median size distributions was typically bimodal, except under polluted conditions when the size distribution was unimodal. During the colder months, the daily variation of particle number size distributions are strongly influenced by a diurnal breeze system, whereby the Aitken and accumulation modes vary similarly to PM1 and BC mass concentrations, with nocturnal minima and sharp day-time increases owing to the development of a diurnal mountain breeze. Under clean air conditions, high levels of nucleation and lower Aitken mode concentrations were measured, highlighting the importance of new particle formation as a source of particles in the absence of a significant condensation sink. During the warmer months, nucleation mode concentrations were observed to be relatively elevated both under polluted and clean conditions due to increased photochemical reactions, with enhanced subsequent growth owing to elevated concentrations of condensable organic vapours produced from biogenic volatile organic compounds, indicating that nucleation at MSY does not exclusively occur under clean air conditions. Finally, mixing of air masses between polluted and non-polluted boundary layer air, and brief changes in the air mass being sampled gave rise to unusual particle number size distributions, with specific cases of such behaviour discussed at length.This study was supported by the Ministry of Economy and Competitiveness and FEDER funds under the projects CARIATI (CGL2008-06294/CLI), VAMOS (CGL2010 19464/CLI) and GRACCIE (CSD 2007-00067), and from the Generalitat de Catalunya 2009 SGR8. The research leading to these results has received funding from the European Union Seventh Framework Programme (FP7/ 2007-2013) ACTRIS under grant agreement no. 262254. The authors would like to extend their gratitude to Jesu´ s Parga and Jordi Gil for their technical support. The authors also thank METEOCAT for the meteorological data and the NOAA Air Resources Laboratory (ARL) for the provision of the HYSPLIT transport and dispersion model and/or READY website (http://www.arl.noaa.gov/ ready.html) used in this publication.Peer reviewedCo-Action PublishingEuropean CommissionConsejo Superior de Investigaciones Científicas [https://ror.org/02gfc7t72]201520152013info:eu-repo/semantics/articlehttp://purl.org/coar/resource_type/c_6501Postprintinfo:eu-repo/semantics/acceptedVersionhttp://hdl.handle.net/10261/122751reponame:DIGITAL.CSIC. Repositorio Institucional del CSICinstname:Consejo Superior de Investigaciones Científicas (CSIC)Inglés#PLACEHOLDER_PARENT_METADATA_VALUE#info:eu-repo/grantAgreement /EC/FP7/65410910.3402/tellusb.v65i0.19243Síinfo:eu-repo/semantics/openAccessoai:digital.csic.es:10261/1227512026-05-22T06:33:51Z |
| dc.title.none.fl_str_mv |
Variability of sub-micrometer particle number size distributions and concentrations in the Western Mediterranean regional background |
| title |
Variability of sub-micrometer particle number size distributions and concentrations in the Western Mediterranean regional background |
| spellingShingle |
Variability of sub-micrometer particle number size distributions and concentrations in the Western Mediterranean regional background Cusack, Michael Nucleation Number concentration Photochemistry Western Mediterranean Sub-micrometer particle size distribution |
| title_short |
Variability of sub-micrometer particle number size distributions and concentrations in the Western Mediterranean regional background |
| title_full |
Variability of sub-micrometer particle number size distributions and concentrations in the Western Mediterranean regional background |
| title_fullStr |
Variability of sub-micrometer particle number size distributions and concentrations in the Western Mediterranean regional background |
| title_full_unstemmed |
Variability of sub-micrometer particle number size distributions and concentrations in the Western Mediterranean regional background |
| title_sort |
Variability of sub-micrometer particle number size distributions and concentrations in the Western Mediterranean regional background |
| dc.creator.none.fl_str_mv |
Cusack, Michael Pérez, Noemí Pey, Jorge Wiedensohler, Alfred Alastuey, Andrés Querol, Xavier |
| author |
Cusack, Michael |
| author_facet |
Cusack, Michael Pérez, Noemí Pey, Jorge Wiedensohler, Alfred Alastuey, Andrés Querol, Xavier |
| author_role |
author |
| author2 |
Pérez, Noemí Pey, Jorge Wiedensohler, Alfred Alastuey, Andrés Querol, Xavier |
| author2_role |
author author author author author |
| dc.contributor.none.fl_str_mv |
European Commission Consejo Superior de Investigaciones Científicas [https://ror.org/02gfc7t72] |
| dc.subject.none.fl_str_mv |
Nucleation Number concentration Photochemistry Western Mediterranean Sub-micrometer particle size distribution |
| topic |
Nucleation Number concentration Photochemistry Western Mediterranean Sub-micrometer particle size distribution |
| description |
This study focuses on the daily and seasonal variability of particle number size distributions and concentrations, performed at the Montseny (MSY) regional background station in the western Mediterranean from October 2010 to June 2011. Particle number concentrations at MSY were shown to be within range of various other sites across Europe reported in literature, but the seasonality of the particle number size distributions revealed significant differences. The Aitken mode is the dominant particle mode at MSY, with arithmetic mean concentrations of 1698 cm3, followed by the accumulation mode (877 cm-3) and the nucleation mode (246 cm-3). Concentrations showed a strong seasonal variability with large increases in particle number concentrations observed from the colder to warmer months. The modality of median size distributions was typically bimodal, except under polluted conditions when the size distribution was unimodal. During the colder months, the daily variation of particle number size distributions are strongly influenced by a diurnal breeze system, whereby the Aitken and accumulation modes vary similarly to PM1 and BC mass concentrations, with nocturnal minima and sharp day-time increases owing to the development of a diurnal mountain breeze. Under clean air conditions, high levels of nucleation and lower Aitken mode concentrations were measured, highlighting the importance of new particle formation as a source of particles in the absence of a significant condensation sink. During the warmer months, nucleation mode concentrations were observed to be relatively elevated both under polluted and clean conditions due to increased photochemical reactions, with enhanced subsequent growth owing to elevated concentrations of condensable organic vapours produced from biogenic volatile organic compounds, indicating that nucleation at MSY does not exclusively occur under clean air conditions. Finally, mixing of air masses between polluted and non-polluted boundary layer air, and brief changes in the air mass being sampled gave rise to unusual particle number size distributions, with specific cases of such behaviour discussed at length. |
| publishDate |
2013 |
| dc.date.none.fl_str_mv |
2013 2015 2015 |
| dc.type.none.fl_str_mv |
info:eu-repo/semantics/article http://purl.org/coar/resource_type/c_6501 Postprint info:eu-repo/semantics/acceptedVersion |
| format |
article |
| status_str |
acceptedVersion |
| dc.identifier.none.fl_str_mv |
http://hdl.handle.net/10261/122751 |
| url |
http://hdl.handle.net/10261/122751 |
| dc.language.none.fl_str_mv |
Inglés |
| language_invalid_str_mv |
Inglés |
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#PLACEHOLDER_PARENT_METADATA_VALUE# info:eu-repo/grantAgreement /EC/FP7/654109 10.3402/tellusb.v65i0.19243 Sí |
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info:eu-repo/semantics/openAccess |
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openAccess |
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Co-Action Publishing |
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Co-Action Publishing |
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reponame:DIGITAL.CSIC. Repositorio Institucional del CSIC instname:Consejo Superior de Investigaciones Científicas (CSIC) |
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Consejo Superior de Investigaciones Científicas (CSIC) |
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DIGITAL.CSIC. Repositorio Institucional del CSIC |
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DIGITAL.CSIC. Repositorio Institucional del CSIC |
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1869424340044349440 |
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15.81155 |