<?xml version='1.0' encoding='utf-8'?>
<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:contributor>Sasha C. Reed</dc:contributor>
  <dc:contributor>Kelly M. Andersen</dc:contributor>
  <dc:contributor>Damla Cinoğlu</dc:contributor>
  <dc:contributor>Matthew E. Craig</dc:contributor>
  <dc:contributor>Lee H. Dietterich</dc:contributor>
  <dc:contributor>J.A. Hogan</dc:contributor>
  <dc:contributor>Jennifer A. Holmes</dc:contributor>
  <dc:contributor>Andrew T. Nottingham</dc:contributor>
  <dc:contributor>Rebecca Ostertag</dc:contributor>
  <dc:contributor>Fiona M. Soper</dc:contributor>
  <dc:contributor>Tana E. Wood</dc:contributor>
  <dc:contributor>Michelle Y. Wong</dc:contributor>
  <dc:creator>Daniela F. Cusack</dc:creator>
  <dc:date>2024</dc:date>
  <dc:description>&lt;p&gt;&lt;span&gt;Tropical forests play a critical role in the global carbon (C) cycle. These ecosystems maintain the highest rates of net primary production (NPP) on Earth (Hengl&amp;nbsp;&lt;/span&gt;&lt;i&gt;et&amp;nbsp;al&lt;/i&gt;&lt;span&gt;.,&amp;nbsp;&lt;/span&gt;&lt;span&gt;&lt;a id="#nph19511-bib-0014_R_d6461774e632" class="bibLink tab-link" href="https://nph.onlinelibrary.wiley.com/doi/10.1111/nph.19511#nph19511-bib-0014" data-tab="pane-pcw-references" data-mce-href="https://nph.onlinelibrary.wiley.com/doi/10.1111/nph.19511#nph19511-bib-0014"&gt;2017&lt;/a&gt;&lt;/span&gt;&lt;span&gt;), contain&amp;nbsp;&lt;/span&gt;&lt;i&gt;c&lt;/i&gt;&lt;span&gt;. 30% of terrestrial C stocks (Jobbagy &amp;amp; Jackson,&amp;nbsp;&lt;/span&gt;&lt;span&gt;&lt;a id="#nph19511-bib-0020_R_d6461774e637" class="bibLink tab-link" href="https://nph.onlinelibrary.wiley.com/doi/10.1111/nph.19511#nph19511-bib-0020" data-tab="pane-pcw-references" data-mce-href="https://nph.onlinelibrary.wiley.com/doi/10.1111/nph.19511#nph19511-bib-0020"&gt;2000&lt;/a&gt;&lt;/span&gt;&lt;span&gt;), and have some of the largest stores of fine-root biomass globally (Jackson&amp;nbsp;&lt;/span&gt;&lt;i&gt;et&amp;nbsp;al&lt;/i&gt;&lt;span&gt;.,&amp;nbsp;&lt;/span&gt;&lt;span&gt;&lt;a id="#nph19511-bib-0019_R_d6461774e643" class="bibLink tab-link" href="https://nph.onlinelibrary.wiley.com/doi/10.1111/nph.19511#nph19511-bib-0019" data-tab="pane-pcw-references" data-mce-href="https://nph.onlinelibrary.wiley.com/doi/10.1111/nph.19511#nph19511-bib-0019"&gt;1996&lt;/a&gt;&lt;/span&gt;&lt;span&gt;), as well as higher fine-root production and turnover rates compared with other biomes (Cusack&amp;nbsp;&lt;/span&gt;&lt;i&gt;et&amp;nbsp;al&lt;/i&gt;&lt;span&gt;.,&amp;nbsp;&lt;/span&gt;&lt;span&gt;&lt;a id="#nph19511-bib-0007_R_d6461774e648" class="bibLink tab-link" href="https://nph.onlinelibrary.wiley.com/doi/10.1111/nph.19511#nph19511-bib-0007" data-tab="pane-pcw-references" data-mce-href="https://nph.onlinelibrary.wiley.com/doi/10.1111/nph.19511#nph19511-bib-0007"&gt;2021&lt;/a&gt;&lt;/span&gt;&lt;span&gt;). Tropical forest responses to projected warming, altered rainfall regimes, and elevated CO&lt;/span&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;span&gt;&amp;nbsp;concentrations (IPCC,&amp;nbsp;&lt;/span&gt;&lt;span&gt;&lt;a id="#nph19511-bib-0018_R_d6461774e653" class="bibLink tab-link" href="https://nph.onlinelibrary.wiley.com/doi/10.1111/nph.19511#nph19511-bib-0018" data-tab="pane-pcw-references" data-mce-href="https://nph.onlinelibrary.wiley.com/doi/10.1111/nph.19511#nph19511-bib-0018"&gt;2021&lt;/a&gt;&lt;/span&gt;&lt;span&gt;) are likely to be different from other ecosystems because of their unique characteristics (Box&amp;nbsp;&lt;/span&gt;&lt;a class="featureLink scrollableLink" title="Link to feature" href="https://nph.onlinelibrary.wiley.com/doi/10.1111/nph.19511#nph19511-fea-0001" data-mce-href="https://nph.onlinelibrary.wiley.com/doi/10.1111/nph.19511#nph19511-fea-0001"&gt;1&lt;/a&gt;&lt;span&gt;), making targeted research and model development important for understanding tropical forest–climate feedbacks. There is now a critical mass of long-term global change field experiments and modeling efforts in tropical forests, yet thus far there has been little synthesis, cross-site comparison, or multi-site standardized experimentation among tropical forests to help us understand how these biomes are changing. An organized INSPIRE session at the 108&lt;/span&gt;&lt;sup&gt;th&lt;/sup&gt;&lt;span&gt;&amp;nbsp;Annual Meeting of the Ecological Society of America set out to tackle just this. Speakers covered large-scale tropical forest field experiments and modeling efforts, with an emphasis on changes in ecosystem biogeochemistry under warming, drying, elevated atmospheric CO&lt;/span&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;span&gt;, and changing nutrient status. In this Meeting report, we provide an overview of the large-scale global change experiments presented and highlight the main objectives and opportunities for tropical forest research that emerged, including cross-site comparisons and integration with ecosystem-scale models (Fig.&amp;nbsp;&lt;/span&gt;&lt;a href="https://nph.onlinelibrary.wiley.com/doi/10.1111/nph.19511#nph19511-fig-0001" data-mce-href="https://nph.onlinelibrary.wiley.com/doi/10.1111/nph.19511#nph19511-fig-0001"&gt;1&lt;/a&gt;&lt;span&gt;).&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1111/nph.19511</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>New Phytologist Foundation</dc:publisher>
  <dc:title>Tropical forests and global change: Biogeochemical responses and opportunities for cross-site comparisons, an organized INSPIRE session at the 108th Annual Meeting, Ecological Society of America, Portland, Oregon, USA, August 2023</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>