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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-2025-5267</article-id>
<title-group>
<article-title>Global and Regional Impacts of Forest Expansion on Future Wildfires</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>King</surname>
<given-names>James A.</given-names>
<ext-link>https://orcid.org/0000-0001-8825-0183</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>Simpson</surname>
<given-names>Kimberley J.</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>Bousfield</surname>
<given-names>Christopher G.</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>Val Martin</surname>
<given-names>Maria</given-names>
<ext-link>https://orcid.org/0000-0001-9715-0504</ext-link>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Leverhulme Centre for Climate Change Mitigation, School of Biosciences, University of Sheffield, Sheffield, UK</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Ecology and Evolutionary Biology, School of Biosciences, University of Sheffield, Sheffield, UK</addr-line>
</aff>
<pub-date pub-type="epub">
<day>12</day>
<month>11</month>
<year>2025</year>
</pub-date>
<volume>2025</volume>
<fpage>1</fpage>
<lpage>33</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2025 James A. King 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-2025-5267/">This article is available from https://egusphere.copernicus.org/preprints/2025/egusphere-2025-5267/</self-uri>
<self-uri xlink:href="https://egusphere.copernicus.org/preprints/2025/egusphere-2025-5267/egusphere-2025-5267.pdf">The full text article is available as a PDF file from https://egusphere.copernicus.org/preprints/2025/egusphere-2025-5267/egusphere-2025-5267.pdf</self-uri>
<abstract>
<p>Expansion of global forest cover via afforestation, reforestation, and forest restoration is a widely proposed nature-based solution for climate change mitigation, yet its effect on wildfire activity is poorly understood. As anthropogenic climate change intensifies and wildfire regimes change globally, evaluating the interactions between forest expansion, climate and population change is critical. We assess how large-scale forest expansion influences future fire activity and the land carbon sink using the Community Land Model version 5 (CLM5) with a mechanistic fire module. We simulate a maximum forest scenario (~ 750 Mha by 2100) under 2 &amp;deg;C and 4 &amp;deg;C warming pathways and compare it to three different land use trajectories with varying levels of forest cover and population change. We find that tropical forest expansion decreases fire activity by halting deforestation fires and replacing flammable grasslands with less flammable tree cover. In contrast, temperate forest expansion, such as in the Mediterranean, central Asia and continental US, can more than double fire carbon emissions under high warming, due to drier conditions and increased fuel loads. Population changes also influence fire regimes, with rising population growth in sub-Saharan Africa suppressing fire and reducing burned area, while decreasing populations in Europe and parts of East Asia are associated with increased fire activity. Finally, fires reduce the global land carbon sink by up to ~ 60 PgC by 2100, equivalent to ~ 5.6 times present-day annual CO&lt;sub&gt;2&lt;/sub&gt; emissions, emphasising the need to incorporate fire into climate mitigation planning. Our results suggest that forest expansion can both reduce and intensify fire risk depending on location and that fire-climate-land-human feedbacks must be accounted for in nature-based CO&lt;sub&gt;2&lt;/sub&gt; mitigation strategies.</p>
</abstract>
<counts><page-count count="33"/></counts>
<funding-group>
<award-group id="gs1">
<funding-source>UK Research and Innovation</funding-source>
<award-id>MR/T019867/1</award-id>
</award-group>
</funding-group>
</article-meta>
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