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        <datestamp>2025-04-23T12:12:26Z</datestamp>
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          <identifier identifierType="DOI">10.5522/04/28846736.v2</identifier>
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            <creator>
              <creatorName>Horner, Rebekah</creatorName>
              <givenName>Rebekah</givenName>
              <familyName>Horner</familyName>
            </creator>
            <creator>
              <creatorName>Marais, Eloise</creatorName>
              <givenName>Eloise</givenName>
              <familyName>Marais</familyName>
              <nameIdentifier nameIdentifierScheme="ORCID" schemeURI="http://orcid.org">0000-0001-5477-8051</nameIdentifier>
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          <titles>
            <title><![CDATA[Free tropospheric nitrogen dioxide concentrations from cloud-slicing TROPOMI]]></title>
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          <subjects>
            <subject>Atmospheric composition, chemistry and processes</subject>
            <subject>TROPOMI</subject>
            <subject>cloud-slicing</subject>
            <subject>free troposphere</subject>
            <subject>NO2</subject>
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          <dates>
            <date dateType="Created">2025-08-01</date>
            <date dateType="Updated">2025-08-01</date>
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          <resourceType resourceTypeGeneral="Dataset">Dataset</resourceType>
          <publicationYear>2025</publicationYear>
          <publisher>University College London</publisher>
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            <description descriptionType="Abstract"><![CDATA[<p dir="ltr">Seasonal multiyear mean nitrogen dioxide (NO<sub>2</sub>) mixing ratios in the free troposphere (300-700 hPa) obtained by applying cloud-slicing to total column densities of NO<sub>2</sub> from the TROPOspheric Monitoring Instrument (TROPOMI). </p><p dir="ltr">Years averaged over are given in the filenames. Data are global coverage on a 1 degree horizontal grid. </p><p dir="ltr">The cloud-slicing technique is mostly consistent with the approach detailed in the open access, peer-reviewed <a href="https://acp.copernicus.org/articles/24/13047/2024/acp-24-13047-2024.pdf" rel="noreferrer" target="_blank">Horner et al. (2024)</a> paper, except that the target pressure range is 300-700 hPa to cover the full extent of the free troposphere and filtering to remove cloud-sliced NO<sub>2</sub> data that fall statistically below zero is relaxed from (slope_error + slope) to (2*slope_error + slope), where the slope is the Theil-Sen regression slope obtained from regressing cloud top heights and total NO<sub>2</sub> columns above optically thick clouds. These methodological adjustments are made for comparison to cloud-sliced NO<sub>2</sub> obtained from the geostationary Tropospheric Emissions: Monitoring of Pollution (TEMPO) that has a limited viewing domain covering North America.</p>]]></description>
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