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<front>
<journal-meta>
<journal-id journal-id-type="publisher">ACP</journal-id>
<journal-title-group>
<journal-title>Atmospheric Chemistry and Physics</journal-title>
<abbrev-journal-title abbrev-type="publisher">ACP</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Atmos. Chem. Phys.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7324</issn>
<publisher><publisher-name>Copernicus Publications</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acp-15-5929-2015</article-id>
<title-group>
<article-title>Traffic and nucleation events as main sources of ultrafine particles in high-insolation developed world cities</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Brines</surname>
<given-names>M.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Dall'Osto</surname>
<given-names>M.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Beddows</surname>
<given-names>D. C. S.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Harrison</surname>
<given-names>R. M.</given-names>
<ext-link>https://orcid.org/0000-0002-2684-5226</ext-link>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Gómez-Moreno</surname>
<given-names>F.</given-names>
</name>
<xref ref-type="aff" rid="aff6">
<sup>6</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Núñez</surname>
<given-names>L.</given-names>
</name>
<xref ref-type="aff" rid="aff6">
<sup>6</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Artíñano</surname>
<given-names>B.</given-names>
</name>
<xref ref-type="aff" rid="aff6">
<sup>6</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Costabile</surname>
<given-names>F.</given-names>
</name>
<xref ref-type="aff" rid="aff7">
<sup>7</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Gobbi</surname>
<given-names>G. P.</given-names>
</name>
<xref ref-type="aff" rid="aff7">
<sup>7</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Salimi</surname>
<given-names>F.</given-names>
</name>
<xref ref-type="aff" rid="aff8">
<sup>8</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Morawska</surname>
<given-names>L.</given-names>
<ext-link>https://orcid.org/0000-0002-0594-9683</ext-link>
</name>
<xref ref-type="aff" rid="aff8">
<sup>8</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Sioutas</surname>
<given-names>C.</given-names>
</name>
<xref ref-type="aff" rid="aff9">
<sup>9</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Querol</surname>
<given-names>X.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Institute of Environmental Assessment and Water Research (ID&amp;AElig;A) Consejo Superior de Investigaciones Científicas (CSIC), C/ Jordi Girona 18–26, 08034 Barcelona, Spain</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Department of Astronomy and Meteorology, Faculty of Physics, University of Barcelona, C/ Martí i Franquès 1, 08028 Barcelona, Spain</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Institute of Marine Sciences (ICM) Consejo Superior de Investigaciones Científicas (CSIC), Pg. Marítim de la Barceloneta 37–49, 08003 Barcelona, Spain</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>National Centre for Atmospheric Science Division of Environmental Health &amp; Risk Management School of Geography, Earth &amp; Environmental Sciences, University of Birmingham, Edgbaston, Birmingham, B15 2TT, United Kingdom</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>Department of Environmental Sciences/Center of Excellence in Environmental Studies, King Abdulaziz University, Jeddah, 21589, Saudi Arabia</addr-line>
</aff>
<aff id="aff6">
<label>6</label>
<addr-line>CIEMAT, Environment Department, Unidad Asociada CSIC-CIEMAT, Av. Complutense 40, 28040 Madrid, Spain</addr-line>
</aff>
<aff id="aff7">
<label>7</label>
<addr-line>CNR – Institute for Atmospheric Sciences and Climate, via Fosso del Cavaliere, 100, Rome, Italy</addr-line>
</aff>
<aff id="aff8">
<label>8</label>
<addr-line>International Laboratory of Air Quality and Health, Queensland University of Technology, G.P.O. Box 2434, Brisbane QLD 4001, Australia</addr-line>
</aff>
<aff id="aff9">
<label>9</label>
<addr-line>University of Southern California, Sonny Astani Department of Civil and Environmental Engineering, 3620 S Vermont Ave., Los Angeles, CA, 90089, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>28</day>
<month>05</month>
<year>2015</year>
</pub-date>
<volume>15</volume>
<issue>10</issue>
<fpage>5929</fpage>
<lpage>5945</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2015 M. Brines et al.</copyright-statement>
<copyright-year>2015</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution 3.0 Unported License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by/3.0/">https://creativecommons.org/licenses/by/3.0/</ext-link></license-p>
</license>
</permissions>
<self-uri xlink:href="https://acp.copernicus.org/articles/15/5929/2015/acp-15-5929-2015.html">This article is available from https://acp.copernicus.org/articles/15/5929/2015/acp-15-5929-2015.html</self-uri>
<self-uri xlink:href="https://acp.copernicus.org/articles/15/5929/2015/acp-15-5929-2015.pdf">The full text article is available as a PDF file from https://acp.copernicus.org/articles/15/5929/2015/acp-15-5929-2015.pdf</self-uri>
<abstract>
<p>Road traffic emissions are often considered the main source of ultrafine
particles (UFP, diameter smaller than 100 nm) in urban environments.
However, recent studies worldwide have shown that – in high-insolation urban
regions at least – new particle formation events can also contribute to UFP.
In order to quantify such events we systematically studied three cities
located in predominantly sunny environments: Barcelona (Spain), Madrid
(Spain) and Brisbane (Australia). Three long-term data sets (1–2 years) of
fine and ultrafine particle number size distributions (measured by SMPS,
Scanning Mobility Particle Sizer) were analysed. Compared to total particle
number concentrations, aerosol size distributions offer far more information
on the type, origin and atmospheric evolution of the particles. By applying
&lt;i&gt;k&lt;/i&gt;-means clustering analysis, we categorized the collected aerosol size
distributions into three main categories: &quot;Traffic&quot; (prevailing 44–63% of
the time), &quot;Nucleation&quot; (14–19%) and &quot;Background pollution and
Specific cases&quot; (7–22%). Measurements from Rome (Italy) and Los Angeles
(USA) were also included to complement the study. The daily variation
of the average UFP concentrations for a typical nucleation day at each site
revealed a similar pattern for all cities, with three distinct particle
bursts. A morning and an evening spike reflected traffic rush hours, whereas
a third one at midday showed nucleation events. The photochemically
nucleated particles&apos; burst lasted 1–4 h, reaching sizes of 30–40 nm. On
average, the occurrence of particle size spectra dominated by nucleation
events was 16% of the time, showing the importance of this process as a
source of UFP in urban environments exposed to high solar radiation. Nucleation events lasting for 2 h or more occurred on 55% of
the days, this extending to &gt; 4 h in 28% of the days,
demonstrating that atmospheric conditions in urban environments are not
favourable to the growth of photochemically nucleated particles. In summary,
although traffic remains the main source of UFP in urban areas, in developed
countries with high insolation urban nucleation events are also a main
source of UFP. If traffic-related particle concentrations are reduced in the
future, nucleation events will likely increase in urban areas, due to the
reduced urban condensation sinks.</p>
</abstract>
<counts><page-count count="17"/></counts>
</article-meta>
</front>
<body/>
<back>
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