<?xml version="1.0" encoding="UTF-8"?>
<!DOCTYPE article PUBLIC "-//NLM//DTD Journal Publishing DTD v3.0 20080202//EN" "https://jats.nlm.nih.gov/nlm-dtd/publishing/3.0/journalpublishing3.dtd">
<article xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" article-type="data-paper" specific-use="SMUR" dtd-version="3.0" xml:lang="en">
<front>
<journal-meta>
<journal-id journal-id-type="publisher">ESSDD</journal-id>
<journal-title-group>
<journal-title>Earth System Science Data Discussions</journal-title>
<abbrev-journal-title abbrev-type="publisher">ESSDD</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Earth Syst. Sci. Data Discuss.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1866-3591</issn>
<publisher><publisher-name></publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/essd-2026-490</article-id>
<title-group>
<article-title>Thirteen years of aerosol chemical composition measurements in the Paris region: reprocessing and applications</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Brochet</surname>
<given-names>Juliette</given-names>
<ext-link>https://orcid.org/0009-0009-9418-6021</ext-link>
</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>Chebaicheb</surname>
<given-names>Hasna</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</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>Favez</surname>
<given-names>Olivier</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</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>Cadeo</surname>
<given-names>Laura</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>Amodeo</surname>
<given-names>Tanguy</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Zhang</surname>
<given-names>Yunjiang</given-names>
<ext-link>https://orcid.org/0000-0002-4361-9685</ext-link>
</name>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Bergé</surname>
<given-names>Antonin</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>Croteau</surname>
<given-names>Philip</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>Crenn</surname>
<given-names>Vincent</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>Gros</surname>
<given-names>Valérie</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Petit</surname>
<given-names>Jean-Eudes</given-names>
<ext-link>https://orcid.org/0000-0003-1516-5927</ext-link>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Laboratoire des Sciences du Climat et de l’Environnement (LSCE), CEA, CNRS, UVSQ, Université Paris-Saclay, Gif-sur-Yvette, France</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Aerosol Chemical Monitor Calibration Centre (ACMCC), CEA/Orme des Merisiers, Gif-sur-Yvette, France</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Institut National de l’Environnement Industriel et des Risques (INERIS), Verneuil-en-Halatte, France</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>University of Milan, Milan, Italy</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>Nanjing University of Information Science and Technology (NUIST), Nanjing, Jiangsu, China</addr-line>
</aff>
<aff id="aff6">
<label>6</label>
<addr-line>Aerodyne Research, Inc, Billerica, Massachusetts, USA</addr-line>
</aff>
<aff id="aff7">
<label>7</label>
<addr-line>ADDAIR, Buc, France</addr-line>
</aff>
<pub-date pub-type="epub">
<day>11</day>
<month>08</month>
<year>2026</year>
</pub-date>
<volume>2026</volume>
<fpage>1</fpage>
<lpage>28</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2026 Juliette Brochet et al.</copyright-statement>
<copyright-year>2026</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution 4.0 International License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by/4.0/">https://creativecommons.org/licenses/by/4.0/</ext-link></license-p>
</license>
</permissions>
<self-uri xlink:href="https://essd.copernicus.org/preprints/essd-2026-490/">This article is available from https://essd.copernicus.org/preprints/essd-2026-490/</self-uri>
<self-uri xlink:href="https://essd.copernicus.org/preprints/essd-2026-490/essd-2026-490.pdf">The full text article is available as a PDF file from https://essd.copernicus.org/preprints/essd-2026-490/essd-2026-490.pdf</self-uri>
<abstract>
<p>The recent development of very long-term Aerosol Chemical Speciation Monitor (ACSM) time series presents new insights into the spatiotemporal variability of atmospheric submicron aerosol (PM&lt;sub&gt;1&lt;/sub&gt;) composition. However, challenges in analyzing long-term datasets remain due to their discontinuities. This study proposes a new methodology to homogenize long-term features monitored at the semi-urban SIRTA observatory, located in the Paris region, and then analyzes the variability of the reprocessed dataset, which can be found in EBAS database at &lt;a href=&quot;https://doi.org/10.48597/4RKH-6RDU&quot; target=&quot;_blank&quot; rel=&quot;noopener&quot;&gt;https://doi.org/10.48597/4RKH-6RDU&lt;/a&gt; (Petit, J.-E. and Brochet, J. and ACTRIS and GAW-WDCA, 2025). Response factor (RF) and relative ionization efficiencies (RIEs) have been identified as major parameters to reevaluate, as the concentrations of aerosol are most sensitive to these parameters. Secondly, corrections of ion transmission and mass calibration present a smaller, yet significant, interest in the harmonization protocol. This approach shows a good consistency with the latest standard operation protocol and encouraging results when compared to previous studies. Long-term datasets allow the evaluation of parameterizations like the composition-dependent collection efficiency (CDCE) determined by Middlebrook et al. (2012). In this case, the SIRTA dataset shows good correlation with the CDCE equations, as they stay in their data inter-quartile range, despite the lack of extreme concentration values recorded at the SIRTA observatory. However, this study shows better data consistency with a default collection efficiency (CE) of 0.5 rather than 0.45.&lt;/p&gt;
&lt;p&gt;From 2012 to 2024, PM&lt;sub&gt;1&lt;/sub&gt; have decreased by 3 &lt;em&gt;&amp;mu;&lt;/em&gt;g/m&lt;sup&gt;3&lt;/sup&gt;/yr. Within PM&lt;sub&gt;1&lt;/sub&gt; components, NH&lt;sub&gt;4&lt;/sub&gt; and SO&lt;sub&gt;4&lt;/sub&gt; are significantly decreasing at the annual and seasonal scale, in Autumn (NH&lt;sub&gt;4&lt;/sub&gt; -0.050 and -0.053 &lt;em&gt;&amp;mu;&lt;/em&gt;g/m&lt;sup&gt;3&lt;/sup&gt;/yr, SO&lt;sub&gt;4&lt;/sub&gt; -0.044 and -0.046 &lt;em&gt;&amp;mu;&lt;/em&gt;g/m&lt;sup&gt;3&lt;/sup&gt;/yr respectively). Spring, with the highest PM&lt;sub&gt;1&lt;/sub&gt; concentrations, demonstrates significant decreasing trends for the majority of PM&lt;sub&gt;1&lt;/sub&gt; components (OM -0.21 &lt;em&gt;&amp;mu;&lt;/em&gt;g/m&lt;sup&gt;3&lt;/sup&gt;/yr, NO&lt;sub&gt;3&lt;/sub&gt; -0.23 &lt;em&gt;&amp;mu;&lt;/em&gt;g/m&lt;sup&gt;3&lt;/sup&gt;/yr, NH&lt;sub&gt;4&lt;/sub&gt; -0.12 &lt;em&gt;&amp;mu;&lt;/em&gt;g/m&lt;sup&gt;3&lt;/sup&gt;/yr and SO&lt;sub&gt;4&lt;/sub&gt; -0.093 &lt;em&gt;&amp;mu;&lt;/em&gt;g/m&lt;sup&gt;3&lt;/sup&gt;/yr). Compared with the original dataset, these results highlight the critical importance of harmonized reprocessing for the analysis of very long-term features. Persistent Pollution Episodes (PPE) also have a decreasing trend of occurrence (5 % per year) and might correlate between their duration and maximum concentrations. These trends are placed in the context of synoptic weather regimes, in which blocking regimes dominate the formation of PPE. Finally, the long-term measurements of SO&lt;sub&gt;4&lt;/sub&gt; at SIRTA reveal the need for S-related source apportionment analysis, through the identification of the contributions of volcanic and marine biogenic aerosols. Overall, with the general reduction in atmospheric aerosol concentrations, this study shows encouraging results for air quality, emphasizing the need to maintain mitigation efforts in the Paris region.</p>
</abstract>
<counts><page-count count="28"/></counts>
</article-meta>
</front>
<body/>
<back>
</back>
</article>