Formation and growth of atmospheric nanoparticles in the eastern Mediterranean: results from long-term measurements and process simulations

<p>Atmospheric new particle formation (NPF) is a common phenomenon all over the world. In this study we present the longest time series of NPF records in the eastern Mediterranean region by analyzing 10 years of aerosol number size distribution data obtained with a mobility particle sizer. The...

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Main Authors: N. Kalivitis, V.-M. Kerminen, G. Kouvarakis, I. Stavroulas, E. Tzitzikalaki, P. Kalkavouras, N. Daskalakis, S. Myriokefalitakis, A. Bougiatioti, H. E. Manninen, P. Roldin, T. Petäjä, M. Boy, M. Kulmala, M. Kanakidou, N. Mihalopoulos
Format: Article
Language:English
Published: Copernicus Publications 2019-03-01
Series:Atmospheric Chemistry and Physics
Online Access:https://www.atmos-chem-phys.net/19/2671/2019/acp-19-2671-2019.pdf
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author N. Kalivitis
N. Kalivitis
V.-M. Kerminen
G. Kouvarakis
I. Stavroulas
I. Stavroulas
I. Stavroulas
E. Tzitzikalaki
P. Kalkavouras
P. Kalkavouras
N. Daskalakis
N. Daskalakis
S. Myriokefalitakis
S. Myriokefalitakis
A. Bougiatioti
H. E. Manninen
H. E. Manninen
P. Roldin
T. Petäjä
M. Boy
M. Kulmala
M. Kanakidou
N. Mihalopoulos
N. Mihalopoulos
spellingShingle N. Kalivitis
N. Kalivitis
V.-M. Kerminen
G. Kouvarakis
I. Stavroulas
I. Stavroulas
I. Stavroulas
E. Tzitzikalaki
P. Kalkavouras
P. Kalkavouras
N. Daskalakis
N. Daskalakis
S. Myriokefalitakis
S. Myriokefalitakis
A. Bougiatioti
H. E. Manninen
H. E. Manninen
P. Roldin
T. Petäjä
M. Boy
M. Kulmala
M. Kanakidou
N. Mihalopoulos
N. Mihalopoulos
Formation and growth of atmospheric nanoparticles in the eastern Mediterranean: results from long-term measurements and process simulations
Atmospheric Chemistry and Physics
author_facet N. Kalivitis
N. Kalivitis
V.-M. Kerminen
G. Kouvarakis
I. Stavroulas
I. Stavroulas
I. Stavroulas
E. Tzitzikalaki
P. Kalkavouras
P. Kalkavouras
N. Daskalakis
N. Daskalakis
S. Myriokefalitakis
S. Myriokefalitakis
A. Bougiatioti
H. E. Manninen
H. E. Manninen
P. Roldin
T. Petäjä
M. Boy
M. Kulmala
M. Kanakidou
N. Mihalopoulos
N. Mihalopoulos
author_sort N. Kalivitis
title Formation and growth of atmospheric nanoparticles in the eastern Mediterranean: results from long-term measurements and process simulations
title_short Formation and growth of atmospheric nanoparticles in the eastern Mediterranean: results from long-term measurements and process simulations
title_full Formation and growth of atmospheric nanoparticles in the eastern Mediterranean: results from long-term measurements and process simulations
title_fullStr Formation and growth of atmospheric nanoparticles in the eastern Mediterranean: results from long-term measurements and process simulations
title_full_unstemmed Formation and growth of atmospheric nanoparticles in the eastern Mediterranean: results from long-term measurements and process simulations
title_sort formation and growth of atmospheric nanoparticles in the eastern mediterranean: results from long-term measurements and process simulations
publisher Copernicus Publications
series Atmospheric Chemistry and Physics
issn 1680-7316
1680-7324
publishDate 2019-03-01
description <p>Atmospheric new particle formation (NPF) is a common phenomenon all over the world. In this study we present the longest time series of NPF records in the eastern Mediterranean region by analyzing 10 years of aerosol number size distribution data obtained with a mobility particle sizer. The measurements were performed at the Finokalia environmental research station on Crete, Greece, during the period June 2008–June 2018. We found that NPF took place on 27&thinsp;% of the available days, undefined days were 23&thinsp;% and non-event days 50&thinsp;%. NPF is more frequent in April and May probably due to the terrestrial biogenic activity and is less frequent in August. Throughout the period under study, nucleation was observed also during the night. Nucleation mode particles had the highest concentration in winter and early spring, mainly because of the minimum sinks, and their average contribution to the total particle number concentration was 8&thinsp;%. Nucleation mode particle concentrations were low outside periods of active NPF and growth, so there are hardly any other local sources of sub-25&thinsp;nm particles. Additional atmospheric ion size distribution data simultaneously collected for more than 2 years were also analyzed. Classification of NPF events based on ion spectrometer measurements differed from the corresponding classification based on a mobility spectrometer, possibly indicating a different representation of local and regional NPF events between these two measurement data sets. We used the MALTE-Box model for simulating a case study of NPF in the eastern Mediterranean region. Monoterpenes contributing to NPF can explain a large fraction of the observed NPF events according to our model simulations. However the adjusted parameterization resulting from our sensitivity tests was significantly different from the initial one that had been determined for the boreal environment.</p>
url https://www.atmos-chem-phys.net/19/2671/2019/acp-19-2671-2019.pdf
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spelling doaj-7df4d3db2c7145caa72346b6232d370c2020-11-24T21:21:34ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242019-03-01192671268610.5194/acp-19-2671-2019Formation and growth of atmospheric nanoparticles in the eastern Mediterranean: results from long-term measurements and process simulationsN. Kalivitis0N. Kalivitis1V.-M. Kerminen2G. Kouvarakis3I. Stavroulas4I. Stavroulas5I. Stavroulas6E. Tzitzikalaki7P. Kalkavouras8P. Kalkavouras9N. Daskalakis10N. Daskalakis11S. Myriokefalitakis12S. Myriokefalitakis13A. Bougiatioti14H. E. Manninen15H. E. Manninen16P. Roldin17T. Petäjä18M. Boy19M. Kulmala20M. Kanakidou21N. Mihalopoulos22N. Mihalopoulos23Environmental Chemical Processes Laboratory, Department of Chemistry, University of Crete, 70013, Heraklion, GreeceInstitute for Astronomy, Astrophysics, Space Applications and Remote Sensing, National Observatory of Athens, I. Metaxa & Vas. Pavlou, 15236 Palea Penteli, GreeceInstitute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, 00014 Helsinki, FinlandEnvironmental Chemical Processes Laboratory, Department of Chemistry, University of Crete, 70013, Heraklion, GreeceEnvironmental Chemical Processes Laboratory, Department of Chemistry, University of Crete, 70013, Heraklion, GreeceEnergy, Environment and Water Research Center, The Cyprus Institute, Nicosia 2121, CyprusInstitute for Environmental Research & Sustainable Development, National Observatory of Athens, I. Metaxa & Vas. Pavlou, 15236 Palea Penteli, GreeceEnvironmental Chemical Processes Laboratory, Department of Chemistry, University of Crete, 70013, Heraklion, GreeceEnvironmental Chemical Processes Laboratory, Department of Chemistry, University of Crete, 70013, Heraklion, GreeceInstitute for Environmental Research & Sustainable Development, National Observatory of Athens, I. Metaxa & Vas. Pavlou, 15236 Palea Penteli, GreeceEnvironmental Chemical Processes Laboratory, Department of Chemistry, University of Crete, 70013, Heraklion, GreeceLaboratory for Modeling and Observation of the Earth System (LAMOS), Institute of Environmental Physics (IUP), University of Bremen, Bremen, GermanyInstitute for Environmental Research & Sustainable Development, National Observatory of Athens, I. Metaxa & Vas. Pavlou, 15236 Palea Penteli, GreeceInstitute for Marine and Atmospheric Research (IMAU), Utrecht, the NetherlandsInstitute for Environmental Research & Sustainable Development, National Observatory of Athens, I. Metaxa & Vas. Pavlou, 15236 Palea Penteli, GreeceInstitute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, 00014 Helsinki, FinlandExperimental Physics Department, CERN, 1211 Geneva, SwitzerlandDivision of Nuclear Physics, Department of Physics, Lund University, P.O.Box 118, 22100 Lund, SwedenInstitute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, 00014 Helsinki, FinlandInstitute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, 00014 Helsinki, FinlandInstitute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, 00014 Helsinki, FinlandEnvironmental Chemical Processes Laboratory, Department of Chemistry, University of Crete, 70013, Heraklion, GreeceEnvironmental Chemical Processes Laboratory, Department of Chemistry, University of Crete, 70013, Heraklion, GreeceInstitute for Environmental Research & Sustainable Development, National Observatory of Athens, I. Metaxa & Vas. Pavlou, 15236 Palea Penteli, Greece<p>Atmospheric new particle formation (NPF) is a common phenomenon all over the world. In this study we present the longest time series of NPF records in the eastern Mediterranean region by analyzing 10 years of aerosol number size distribution data obtained with a mobility particle sizer. The measurements were performed at the Finokalia environmental research station on Crete, Greece, during the period June 2008–June 2018. We found that NPF took place on 27&thinsp;% of the available days, undefined days were 23&thinsp;% and non-event days 50&thinsp;%. NPF is more frequent in April and May probably due to the terrestrial biogenic activity and is less frequent in August. Throughout the period under study, nucleation was observed also during the night. Nucleation mode particles had the highest concentration in winter and early spring, mainly because of the minimum sinks, and their average contribution to the total particle number concentration was 8&thinsp;%. Nucleation mode particle concentrations were low outside periods of active NPF and growth, so there are hardly any other local sources of sub-25&thinsp;nm particles. Additional atmospheric ion size distribution data simultaneously collected for more than 2 years were also analyzed. Classification of NPF events based on ion spectrometer measurements differed from the corresponding classification based on a mobility spectrometer, possibly indicating a different representation of local and regional NPF events between these two measurement data sets. We used the MALTE-Box model for simulating a case study of NPF in the eastern Mediterranean region. Monoterpenes contributing to NPF can explain a large fraction of the observed NPF events according to our model simulations. However the adjusted parameterization resulting from our sensitivity tests was significantly different from the initial one that had been determined for the boreal environment.</p>https://www.atmos-chem-phys.net/19/2671/2019/acp-19-2671-2019.pdf