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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-2025-1396</article-id>
<title-group>
<article-title>Radiative impact of increased middle atmospheric water vapour in the aftermath of the Hunga 2022 volcanic eruption at two locations in the Northern Hemisphere</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Bell</surname>
<given-names>Alistair</given-names>
<ext-link>https://orcid.org/0009-0009-7987-140X</ext-link>
</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>Murk</surname>
<given-names>Axel</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>Stober</surname>
<given-names>Gunter</given-names>
<ext-link>https://orcid.org/0000-0002-7909-6345</ext-link>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Institute of Applied Physics, University of Bern, Bern, Switzerland</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Oeschger Centre for Climate Change Research, University of Bern, Bern, Switzerland</addr-line>
</aff>
<pub-date pub-type="epub">
<day>16</day>
<month>04</month>
<year>2025</year>
</pub-date>
<volume>2025</volume>
<fpage>1</fpage>
<lpage>22</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2025 Alistair Bell 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-2025-1396/">This article is available from https://egusphere.copernicus.org/preprints/2025/egusphere-2025-1396/</self-uri>
<self-uri xlink:href="https://egusphere.copernicus.org/preprints/2025/egusphere-2025-1396/egusphere-2025-1396.pdf">The full text article is available as a PDF file from https://egusphere.copernicus.org/preprints/2025/egusphere-2025-1396/egusphere-2025-1396.pdf</self-uri>
<abstract>
<p>Increases in middle atmosphere water vapour as a result of the 2022 Hunga volcanic eruption have now been detected almost globally, with above-average mixing ratios predicted to persist until around 2032. Changes in the middle atmosphere water vapour volume mixing ratio impact chemical reactions in this section of the atmosphere, can result in more favorable conditions for polar stratospheric and mesospheric cloud formation, and have a significant radiative effect on the middle atmosphere and below. For this reason, precise radiative transfer calculations are important to make accurate and precise assessments of changes to both long-wave and short-wave fluxes, and how this may impact the heating rates at different heights in the atmosphere. In this study, water vapour profiles from two microwave radiometers deployed at two different latitudes in Europe are used to analyse changes in water vapour in the aftermath of the Hunga volcano, and a line-by-line radiative transfer model is used to analyse the thermal impact of this increase over Bern, Switzerland, and Ny-&amp;Aring;lesund, Svalbard.</p>
</abstract>
<counts><page-count count="22"/></counts>
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</front>
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