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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-2026-4705</article-id>
<title-group>
<article-title>Quantifying regional transport contributions and diagnosing ozone formation sensitivity: A trajectory informed machine learning study at background sites across China</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Hu</surname>
<given-names>Baoye</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
<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>Zhao</surname>
<given-names>Yi</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Chen</surname>
<given-names>Naihua</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</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>Xu</surname>
<given-names>Hongkai</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Zeng</surname>
<given-names>Jinfeng</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Chen</surname>
<given-names>Shuyao</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Liu</surname>
<given-names>Yuchao</given-names>
</name>
<xref ref-type="aff" rid="aff6">
<sup>6</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>College of Chemistry, Chemical Engineering and Environment, Minnan Normal University, Zhangzhou, China, 363000</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Fujian Provincial Key Laboratory of Modern Analytical Science and Separation Technology, Minnan Normal University, Zhangzhou, China, 363000</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Fujian Province University Key Laboratory of Pollution Monitoring and Control, Minnan Normal University, Zhangzhou, China, 363000</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Fujian Key Laboratory of Atmospheric Ozone Pollution Prevention, Institute of Urban Environment, Chinese Academy of Sciences, Xiamen 361021, China</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>Pingtan Environmental Monitoring Center of Fujian, Pingtan 350400, China</addr-line>
</aff>
<aff id="aff6">
<label>6</label>
<addr-line>Minnan Normal University, Zhangzhou, China, 363000</addr-line>
</aff>
<pub-date pub-type="epub">
<day>08</day>
<month>09</month>
<year>2026</year>
</pub-date>
<volume>2026</volume>
<fpage>1</fpage>
<lpage>22</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2026 Baoye Hu 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-2026-4705/">This article is available from https://egusphere.copernicus.org/preprints/2026/egusphere-2026-4705/</self-uri>
<self-uri xlink:href="https://egusphere.copernicus.org/preprints/2026/egusphere-2026-4705/egusphere-2026-4705.pdf">The full text article is available as a PDF file from https://egusphere.copernicus.org/preprints/2026/egusphere-2026-4705/egusphere-2026-4705.pdf</self-uri>
<abstract>
<p>Surface ozone (O&lt;sub&gt;3&lt;/sub&gt;) pollution in China is affected by transported pollutants, air mass pathways, local pollution conditions, meteorology, temporal variability, and stratospheric inputs, but their relative roles remain difficult to distinguish at background sites. Here we developed a nationwide trajectory informed machine learning framework to quantify model explained processes controlling hourly O&lt;sub&gt;3&lt;/sub&gt; at 76 background monitoring sites across China during 2015&amp;ndash;2024. Hourly observations were integrated with 72 h HYSPLIT backward trajectories, high resolution gridded pollutant fields along trajectory endpoints, ERA5 meteorology, a CAMS stratospheric O&lt;sub&gt;3&lt;/sub&gt; tracer, and temporal predictors. XGBoost models showed robust performance, with a median test R&lt;sup&gt;2&lt;/sup&gt; of 0.853 across valid station year models. SHAP interpretation showed that trajectory pollutants were the dominant explanatory group, accounting for 56.4 % of the total model explained contribution, followed by ERA5 meteorology, local pollutants, temporal features, trajectory location and height, and stratospheric O&lt;sub&gt;3&lt;/sub&gt;. During MDA8 O&lt;sub&gt;3&lt;/sub&gt; exceedance days (&amp;gt;160 mg m&lt;sup&gt;&amp;minus;3&lt;/sup&gt;), trajectory pollutant contribution increased to 65.3 %, and further to 72.3 % during the peak 8 h window. This enhancement was mainly driven by trajectory O&lt;sub&gt;3&lt;/sub&gt;, whose share within the trajectory pollutant group increased from 75.6 % to 89.3 %. OMI HCHO/NO&lt;sub&gt;2&lt;/sub&gt; ratios indicated that O&lt;sub&gt;3&lt;/sub&gt; formation was mainly VOC limited or transitional. Diurnal analysis further showed that maximum O&lt;sub&gt;3&lt;/sub&gt; was associated with local pollutant meteorology coupling, whereas higher minimum O&lt;sub&gt;3&lt;/sub&gt; reflected transport pathway and background structure. These results highlight the importance of transported O&lt;sub&gt;3&lt;/sub&gt; rich air masses in high O&lt;sub&gt;3&lt;/sub&gt; episodes at Chinese background sites.</p>
</abstract>
<counts><page-count count="22"/></counts>
<funding-group>
<award-group id="gs1">
<funding-source>National Natural Science Foundation of China</funding-source>
<award-id>42305102</award-id>
</award-group>
<award-group id="gs2">
<funding-source>Natural Science Foundation of Fujian Province</funding-source>
<award-id>2023J05179</award-id>
</award-group>
</funding-group>
</article-meta>
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