<?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="research-article" specific-use="SMUR" dtd-version="3.0" xml:lang="en">
<front>
<journal-meta>
<journal-id journal-id-type="publisher">EGUsphere</journal-id>
<journal-title-group>
<journal-title>EGUsphere</journal-title>
<abbrev-journal-title abbrev-type="publisher">EGUsphere</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">EGUsphere</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub"></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/egusphere-2026-2028</article-id>
<title-group>
<article-title>Determination of Aerosol Particle Organic Carbon (OC) by Aerosol Mass Spectrometry (AMS) and Thermo-Optical Transmission (TOT) Analysis: Spatial and Seasonal Differences</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Arora</surname>
<given-names>Shubhi</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>Poulain</surname>
<given-names>Laurent</given-names>
<ext-link>https://orcid.org/0000-0002-9128-7881</ext-link>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Lhotka</surname>
<given-names>Radek</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Vodička</surname>
<given-names>Petr</given-names>
<ext-link>https://orcid.org/0000-0002-9381-3646</ext-link>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Mbengue</surname>
<given-names>Saliou</given-names>
<ext-link>https://orcid.org/0000-0001-7161-3873</ext-link>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Pokorná</surname>
<given-names>Petra</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Schwarz</surname>
<given-names>Jaroslav</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Zíková</surname>
<given-names>Naděžda</given-names>
<ext-link>https://orcid.org/0000-0001-8753-386X</ext-link>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Ondráček</surname>
<given-names>Jakub</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Ždímal</surname>
<given-names>Vladimír</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Herrmann</surname>
<given-names>Hartmut</given-names>
<ext-link>https://orcid.org/0000-0001-7044-2101</ext-link>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Atmospheric Chemistry Department (ACD), Leibniz Institute for Tropospheric Research (TROPOS), Permoserstr. 15,  Leipzig, 04318, Germany</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Institute of Chemical Process Fundamentals, Czech Academy of Sciences, Rozvojová 1/135, Prague, 16500, Czech Republic</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Global Change Research Institute of the Czech Academy of Sciences, 60300, Brno, Czech Republic</addr-line>
</aff>
<pub-date pub-type="epub">
<day>15</day>
<month>07</month>
<year>2026</year>
</pub-date>
<volume>2026</volume>
<fpage>1</fpage>
<lpage>33</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2026 Shubhi Arora 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://egusphere.copernicus.org/preprints/2026/egusphere-2026-2028/">This article is available from https://egusphere.copernicus.org/preprints/2026/egusphere-2026-2028/</self-uri>
<self-uri xlink:href="https://egusphere.copernicus.org/preprints/2026/egusphere-2026-2028/egusphere-2026-2028.pdf">The full text article is available as a PDF file from https://egusphere.copernicus.org/preprints/2026/egusphere-2026-2028/egusphere-2026-2028.pdf</self-uri>
<abstract>
<p>Reliable quantification of organic carbon (OC) is essential for the comparability of long-term aerosol measurements across monitoring networks. A multi-site intercomparison of OC measurements was conducted at three Central European background stations, Melpitz (MEL), Fr&amp;yacute;dlant (FRY), and Ko&amp;scaron;etice (NAOK), using aerosol mass spectrometry (AMS/ACSM) and thermal-optical transmission (TOT) methods (offline and semi-continuous). Semi-continuous and offline TOT measurements showed high consistency across sites and seasons, suggesting negligible influence of particle size differences on OC comparability. A pronounced seasonal contrast was observed between AMS derived OC (OC&lt;sub&gt;AMS&lt;/sub&gt;) and TOT based OC (OC&lt;sub&gt;TOT&lt;/sub&gt;). During summer, good agreement was found with OC&lt;sub&gt;TOT&lt;/sub&gt;:OC&lt;sub&gt;AMS&lt;/sub&gt; slopes of 1.27 (MEL), 0.86 (FRY), and 0.83 (NAOK). In winter, AMS systematically underestimated OC, with slopes decreasing to 0.34 (MEL), 0.24 (FRY), and 0.63 (NAOK). The discrepancy increased under combustion dominated conditions and was associated with low organic aerosol to equivalent black carbon (OA:eBC) ratios (&amp;lt;&amp;asymp;5), identifying a regime where OC&lt;sub&gt;AMS&lt;/sub&gt; and OC&lt;sub&gt;TOT&lt;/sub&gt; diverge substantially. Source dependent effects were evident, with the largest deviations observed at the coal influenced site (FRY) and during long-range transport events, while improved agreement coincided with higher OA:eBC ratios and enhanced secondary organic aerosol formation in summer. Evaluation of potential uncertainties (including pyrolytic carbon formation in TOT and AMS related limitations such as refractory organics and ionization efficiency) showed that no single factor explains the winter discrepancy, suggesting combined matrix and source effects. The results show that OA:eBC can serve as a practical indicator for OC&lt;sub&gt;AMS&lt;/sub&gt;-OC&lt;sub&gt;TOT&lt;/sub&gt; agreement and provide recommendations to improve OC quantification under winter combustion conditions.</p>
</abstract>
<counts><page-count count="33"/></counts>
<funding-group>
<award-group id="gs1">
<funding-source>Deutsche Forschungsgemeinschaft</funding-source>
<award-id>431895563</award-id>
</award-group>
<award-group id="gs2">
<funding-source>Grantová Agentura České Republiky</funding-source>
<award-id>431895563</award-id>
</award-group>
</funding-group>
</article-meta>
</front>
<body/>
<back>
</back>
</article>