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<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-2026-4766</article-id>
<title-group>
<article-title>Primary sources and secondary formation of brown carbon in urban Shanghai: Insights from bihourly measurements of brown carbon and organic tracers</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Wang</surname>
<given-names>Qiongqiong</given-names>
<ext-link>https://orcid.org/0000-0001-8258-7201</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>Huang</surname>
<given-names>Zhongliang</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>Li</surname>
<given-names>Zongjun</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>Zhu</surname>
<given-names>Shuihui</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>Qiao</surname>
<given-names>Liping</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>Zhou</surname>
<given-names>Min</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>Huang</surname>
<given-names>Dandan</given-names>
<ext-link>https://orcid.org/0000-0003-2878-7469</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>Wang</surname>
<given-names>Hongli</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>Fu</surname>
<given-names>Qingyan</given-names>
<ext-link>https://orcid.org/0000-0003-2192-5654</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>Liao</surname>
<given-names>Kezheng</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>Yu</surname>
<given-names>Jian Zhen</given-names>
<ext-link>https://orcid.org/0000-0002-6165-6500</ext-link>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Department of Atmospheric Science, School of Environmental Studies, China University of Geosciences, Wuhan, 430074, China.</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Laboratory of Formation and Prevention of Urban Air Pollution Complex, Ministry of Ecology and Environment, Shanghai Academy of Environmental Sciences, Shanghai 200233, China</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Department of Chemistry, The Hong Kong University of Science and Technology, Hong Kong 999077, China</addr-line>
</aff>
<pub-date pub-type="epub">
<day>18</day>
<month>08</month>
<year>2026</year>
</pub-date>
<volume>2026</volume>
<fpage>1</fpage>
<lpage>21</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2026 Qiongqiong Wang 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-2026-4766/">This article is available from https://egusphere.copernicus.org/preprints/2026/egusphere-2026-4766/</self-uri>
<self-uri xlink:href="https://egusphere.copernicus.org/preprints/2026/egusphere-2026-4766/egusphere-2026-4766.pdf">The full text article is available as a PDF file from https://egusphere.copernicus.org/preprints/2026/egusphere-2026-4766/egusphere-2026-4766.pdf</self-uri>
<abstract>
<p>Brown carbon (BrC) is a significant component of atmospheric carbonaceous aerosols and has important influence on climate, atmospheric chemistry, and air quality. Our knowledge about its sources and atmospheric evolution is limited due to the challenges of accurate estimation of its mass concentrations. To address this gap, we examined concurrent measurements of bihourly BrC and a suite of organic molecular tracers in urban Shanghai from March to August 2020, BrC was determined by synergistically applying the Bayesian inference (BI) model to multi-wavelength aethalometer and total carbon (TC) measurements. BrC constituted 38&amp;ndash;40 % of TC, with pronounced seasonal differences in diurnal evolution. The source apportionment analysis resolved 15 source factors and among them 7 are secondary sources, namely, secondary nitrate and sulfate formation processes, aromatic secondary organic aerosol (SOA), &amp;alpha;-pinene SOA, &amp;beta;-caryophyllene SOA, isoprene SOA, oxygenated cooking OA, and secondary biomass burning. Secondary BrC accounted for 42 % and 49 % of total BrC in spring and summer, respectively. Seasonal contrast of the BrC contributions from primary and secondary sources were noticed. The formation mechanisms of secondary BrC were investigated by isolating events with continuous increment in secondary BrC concentrations, and the analysis suggested the diversity of oxidative pathways governing secondary BrC production. This study demonstrates the potential applicability of coupling the BI framework with online measurements of organic tracers for robust, chemically resolved BrC source apportionment. Our field observations provide the first quantitative source analysis and offer new insights into the primary sources and secondary formation of BrC in the urban atmosphere.</p>
</abstract>
<counts><page-count count="21"/></counts>
<funding-group>
<award-group id="gs1">
<funding-source>National Natural Science Foundation of China</funding-source>
<award-id>42305107</award-id>
<award-id>42307155</award-id>
</award-group>
<award-group id="gs2">
<funding-source>China University of Geosciences</funding-source>
<award-id>2022115</award-id>
</award-group>
<award-group id="gs3">
<funding-source>Research Grants Council, University Grants Committee</funding-source>
<award-id>T24-614/25N</award-id>
</award-group>
</funding-group>
</article-meta>
</front>
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<back>
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