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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-2025-5782</article-id>
<title-group>
<article-title>Ground-based monitoring of nitrogen dioxide in Kumasi, Ghana, and its comparison with satellite observations</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Mijling</surname>
<given-names>Bas</given-names>
<ext-link>https://orcid.org/0000-0003-3101-247X</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>Afotey</surname>
<given-names>Benjamin</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>Eckert</surname>
<given-names>Tim Henrik</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>Mairhofer</surname>
<given-names>Magdalena</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>Gil Pascual</surname>
<given-names>Águeda</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>Yuorkuu</surname>
<given-names>Emmanuel</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>Darko</surname>
<given-names>Philip</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>Amakah</surname>
<given-names>Phiona</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>Boersma</surname>
<given-names>Klaas Folkert</given-names>
<ext-link>https://orcid.org/0000-0002-4591-7635</ext-link>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</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>Asilevi</surname>
<given-names>Prince Junior</given-names>
<ext-link>https://orcid.org/0000-0001-9162-326X</ext-link>
</name>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Royal Netherlands Meteorological Institute (KNMI), De Bilt, 5 3730 AE, the Netherlands</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Department of Chemical Engineering, Kwame Nkrumah University of Science and Technology (KNUST), Kumasi, 00233, Ghana</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Delft University of Technology (TU Delft), Delft, 2600 GA, the Netherlands</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Wageningen University, Meteorology and Air Quality Group, Wageningen, 6700 AA, the Netherlands</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>Department of Meteorology and Climate Science, Kwame Nkrumah University of Science and Technology (KNUST), Kumasi, 00233, Ghana</addr-line>
</aff>
<pub-date pub-type="epub">
<day>07</day>
<month>01</month>
<year>2026</year>
</pub-date>
<volume>2026</volume>
<fpage>1</fpage>
<lpage>29</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2026 Bas Mijling 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-2025-5782/">This article is available from https://egusphere.copernicus.org/preprints/2026/egusphere-2025-5782/</self-uri>
<self-uri xlink:href="https://egusphere.copernicus.org/preprints/2026/egusphere-2025-5782/egusphere-2025-5782.pdf">The full text article is available as a PDF file from https://egusphere.copernicus.org/preprints/2026/egusphere-2025-5782/egusphere-2025-5782.pdf</self-uri>
<abstract>
<p>Air pollution poses an increasing public health risk in many African cities, where systematic monitoring is limited by the high cost of reference-grade instrumentation. Satellite-based sensors such as TROPOMI on Sentinel-5P provide global coverage of atmospheric pollutants, including nitrogen dioxide (NO&lt;sub&gt;2&lt;/sub&gt;), but their limited vertical resolution complicates the estimation of surface-level concentrations.&lt;/p&gt;
&lt;p&gt;Palmes diffusion tubes offer a low-cost, low-tech alternative for measuring NO&lt;sub&gt;2&lt;/sub&gt; at the ground level. Combining satellite observations with data from ground-based diffusion tubes presents a promising approach for generating regional air quality maps, particularly in resource-limited settings. This study reports on the implementation of a pilot network of Palmes tubes in Kumasi, Ghana. To ensure sustainability and scalability, a local air quality laboratory was established to prepare and analyse the tubes using locally sourced materials and equipment.&lt;/p&gt;
&lt;p&gt;Validation against tubes prepared and analysed by an accredited external laboratory demonstrated satisfactory agreement. Measurements from March 2025 revealed a wide range of NO&lt;sub&gt;2&lt;/sub&gt; concentrations, from an average of 7 &amp;micro;g&amp;nbsp;m&lt;sup&gt;-3&lt;/sup&gt; in residential areas away from traffic and industry to peak values of 88 &amp;micro;g&amp;nbsp;m&lt;sup&gt;-3&lt;/sup&gt; at heavily trafficked intersections &amp;ndash; substantially exceeding the WHO 2021 guideline limits of 25 &amp;micro;g m&lt;sup&gt;-3&lt;/sup&gt; for 24-hour exposure and 10 &amp;micro;g&amp;nbsp;m&lt;sup&gt;-3&lt;/sup&gt; for annual mean concentrations.&lt;/p&gt;
&lt;p&gt;Averaged satellite data showed the accumulation of NO₂ plumes downwind of the city, though the relationship with surface-level measurements remains complex and needs further investigation. Column-to-surface ratios in Kumasi are significantly lower than those typically observed in European cities. TROPOMI underestimates the tropospheric NO&lt;sub&gt;2&lt;/sub&gt; column densities by a factor of roughly 2.5 in March 2025, as the higher aerosol loading over Ghana reduces retrieval sensitivity in the troposphere, increasing the reliance on unrepresentative &lt;em&gt;a priori&lt;/em&gt; profiles.</p>
</abstract>
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