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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">1680-7375</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-2025-4464</article-id>
<title-group>
<article-title>The radiative forcing of PM&lt;sub&gt;2.5&lt;/sub&gt; heavy pollution, its influencing factors and importance to precipitation during 2014&amp;ndash;2023 in the Bohai Rim, China</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Zhu</surname>
<given-names>Jun</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>Wang</surname>
<given-names>Yingying</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>Yue</surname>
<given-names>Xu</given-names>
<ext-link>https://orcid.org/0000-0002-8861-8192</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>Che</surname>
<given-names>Huizheng</given-names>
<ext-link>https://orcid.org/0000-0002-9458-3387</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>Xia</surname>
<given-names>Xiangao</given-names>
<ext-link>https://orcid.org/0000-0002-4187-6311</ext-link>
</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>Lu</surname>
<given-names>Xiaofei</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>Tian</surname>
<given-names>Chenguang</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>Liao</surname>
<given-names>Hong</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Jiangsu Key Laboratory of Atmospheric Environment Monitoring and Pollution Control, Collaborative Innovation Center  of Atmospheric Environment and Equipment Technology, School of Environmental Science and Engineering, Nanjing University of Information Science &amp; Technology (NUIST), Nanjing, 210044, China</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>State Key Laboratory of Severe Weather (LASW) and Key Laboratory of Atmospheric Chemistry (LAC), Chinese  Academy of Meteorological Sciences, CMA, Beijing, 100081, China</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>LAGEO, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>University of Chinese Academy of Sciences, Beijing, 100049, China</addr-line>
</aff>
<pub-date pub-type="epub">
<day>17</day>
<month>10</month>
<year>2025</year>
</pub-date>
<volume>2025</volume>
<fpage>1</fpage>
<lpage>27</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2025 Jun Zhu et al.</copyright-statement>
<copyright-year>2025</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/2025/egusphere-2025-4464/">This article is available from https://egusphere.copernicus.org/preprints/2025/egusphere-2025-4464/</self-uri>
<self-uri xlink:href="https://egusphere.copernicus.org/preprints/2025/egusphere-2025-4464/egusphere-2025-4464.pdf">The full text article is available as a PDF file from https://egusphere.copernicus.org/preprints/2025/egusphere-2025-4464/egusphere-2025-4464.pdf</self-uri>
<abstract>
<p>There were PM&lt;sub&gt;2.5&lt;/sub&gt; heavy pollution events in the Bohai Rim regions in China over the past decade, which can significantly affect radiative forcing (RF). However, the characteristics and influencing factors of RF on heavy pollution days, and its relative importance to precipitation remain unclear. This work combined ground-based and satellite observations and reanalysis data to investigate the RF characteristics of regional PM&lt;sub&gt;2.5&lt;/sub&gt; heavy pollution in the Bohai Rim regions during the fall and winter of 2014&amp;ndash;2023. Additionally, the impact of meteorological vertical profiles on surface PM&lt;sub&gt;2.5&lt;/sub&gt; and pollution RF, and the importance of various factors to pollution RF and precipitation, were explored based on machine learning algorithms. The results showed that the RF on PM&lt;sub&gt;2.5&lt;/sub&gt; regional heavy pollution days can be up to approximately -70 Wm&lt;sup&gt;-2&lt;/sup&gt; at the surface, &amp;plusmn;8 Wm&lt;sup&gt;-2&lt;/sup&gt; at top of atmosphere (TOA), and +80 Wm&lt;sup&gt;-2&lt;/sup&gt; in the atmosphere in clear-sky, with lower absolute values in all-sky. Low- to medium-altitude inversions of temperature (T) profiles in the boundary layer favored higher surface PM&lt;sub&gt;2.5&lt;/sub&gt; concentration, whereas isothermal stratification and medium- to high-altitude inversions corresponded to higher surface RF. Lower horizontal speeds and upward motion at low levels can induce higher surface PM&lt;sub&gt;2.5&lt;/sub&gt; and surface RF. Surface PM&lt;sub&gt;2.5&lt;/sub&gt; was the most important factor to surface and atmosphere RF in clear-sky, but V wind in high level (500 hPa) in all-sky. Moreover, pollution RFs in all-sky were as important as vertical winds to the total precipitation. Notably, there was considerable regional heterogeneity in the important factors affecting the RF and precipitation in the Bohai Rim regions.</p>
</abstract>
<counts><page-count count="27"/></counts>
<funding-group>
<award-group id="gs1">
<funding-source>National Natural Science Foundation of China</funding-source>
<award-id>42030608</award-id>
<award-id>42575197</award-id>
</award-group>
</funding-group>
</article-meta>
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