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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-2026-4438</article-id>
<title-group>
<article-title>Contrasting absorption and transport regimes of black and brown carbon across the western, central, and eastern Himalayas</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Shi</surname>
<given-names>Ju-Lian</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="aff8">
<sup>8</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Zhu</surname>
<given-names>Chong-Shu</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff6">
<sup>6</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Qu</surname>
<given-names>Yao</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>Wang</surname>
<given-names>Xiao</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>Wang</surname>
<given-names>Nan</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>Wang</surname>
<given-names>Lu-Yao</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>Dai</surname>
<given-names>Wen-Ting</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff6">
<sup>6</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Huang</surname>
<given-names>Hong</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>Cao</surname>
<given-names>Jun-Ji</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff7">
<sup>7</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>State Key Laboratory of Loess Science, Institute of Earth Environment, Chinese Academy of Sciences, Xi&apos;an 710061, China</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Xi&apos;an Institute for Innovative Earth Environment Research, Xi&apos;an, 710061, China</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>School of Resources and Environment, Nanchang University, Nanchang 330031, China</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Xi&apos;an Meteorological Bureau, Xi&apos;an 710016, China</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>University of Chinese Academy of Sciences, Beijing 100049, China</addr-line>
</aff>
<aff id="aff6">
<label>6</label>
<addr-line>National Field Observation and Research Station (Shaanxi) for Ecological and Environment Changes and Integrated Management in the Guanzhong Plain Region,  Xi&apos;an 710061, China</addr-line>
</aff>
<aff id="aff7">
<label>7</label>
<addr-line>Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China</addr-line>
</aff>
<aff id="aff8">
<label>8</label>
<addr-line>School of Environmental and Municipal Engineering, Xi&apos;an University of Architecture  and Technology, Xi&apos;an 710055, China</addr-line>
</aff>
<pub-date pub-type="epub">
<day>14</day>
<month>09</month>
<year>2026</year>
</pub-date>
<volume>2026</volume>
<fpage>1</fpage>
<lpage>30</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2026 Ju-Lian Shi 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-2026-4438/">This article is available from https://egusphere.copernicus.org/preprints/2026/egusphere-2026-4438/</self-uri>
<self-uri xlink:href="https://egusphere.copernicus.org/preprints/2026/egusphere-2026-4438/egusphere-2026-4438.pdf">The full text article is available as a PDF file from https://egusphere.copernicus.org/preprints/2026/egusphere-2026-4438/egusphere-2026-4438.pdf</self-uri>
<abstract>
<p>Carbonaceous aerosols strongly influence atmospheric radiative forcing over the Himalayas, yet their spatial variability and transport mechanisms remain poorly constrained. Here we present high-time-resolution measurements of black carbon (BC), primary brown carbon (BrC&lt;sub&gt;pri&lt;/sub&gt;), and secondary brown carbon (BrC&lt;sub&gt;sec&lt;/sub&gt;) at three high-altitude sites across the western (Purang), central (Yadong), and eastern (Zay&amp;uuml;) Himalayas during the pre-monsoon period. Distinct spatial gradients in light absorption and biomass burning (BB) tracers (levoglucosan and K⁺) reveal pronounced regional heterogeneity. Yadong exhibits the strongest absorption (B&lt;sub&gt;abs&lt;/sub&gt;: 53.1 &amp;plusmn; 18.5 Mm&lt;sup&gt;&amp;minus;1&lt;/sup&gt; at 370 nm; 14.2 &amp;plusmn; 5.5 Mm&lt;sup&gt;&amp;minus;1&lt;/sup&gt; at 880 nm) and the highest BB influence, indicating a central Himalayan hotspot of polluted aerosol accumulation. BC dominates light absorption across all sites, with its contribution increasing eastward and reaching ~95 % at 660 nm in Zay&amp;uuml;. In contrast, BrC contributions exhibit strong regional contrasts, with BrC&lt;sub&gt;pri&lt;/sub&gt; dominating absorption in Yadong (8&amp;ndash;28 %) and BrC&lt;sub&gt;sec&lt;/sub&gt; enhanced in Purang (3&amp;ndash;26 %). Trajectory analyses indicate that central Himalayan aerosol loading is strongly modulated by orographic uplift and terrain-driven circulation. CALIPSO observations further demonstrate a transition from mineral dust in the west, to pollution-modified dust in the central Himalayas, and biomass-burning aerosols in the east. These results improve our understanding of the sources, transport pathways, and atmospheric transformations of BC, BrC&lt;sub&gt;pri&lt;/sub&gt;, and BrC&lt;sub&gt;sec&lt;/sub&gt; in the Himalayas.</p>
</abstract>
<counts><page-count count="30"/></counts>
<funding-group>
<award-group id="gs1">
<funding-source>National Natural Science Foundation of China</funding-source>
<award-id>42277098</award-id>
<award-id>41771518</award-id>
</award-group>
</funding-group>
</article-meta>
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