<?xml version="1.0" encoding="utf-8"?><feed xmlns="http://www.w3.org/2005/Atom" ><generator uri="https://jekyllrb.com/" version="3.10.0">Jekyll</generator><link href="https://github.com/feed.xml" rel="self" type="application/atom+xml" /><link href="https://github.com/" rel="alternate" type="text/html" /><updated>2026-06-05T13:20:18+00:00</updated><id>https://github.com/feed.xml</id><subtitle>Website for the UKRI-funded Future Leaders Fellowship &quot;PRECOG&quot; (PREdicting biological Carbon in the Ocean Globally)</subtitle><entry><title type="html">Wilson et al., (2022) PNAS</title><link href="https://github.com/Wilson2022/" rel="alternate" type="text/html" title="Wilson et al., (2022) PNAS" /><published>2025-12-05T00:00:00+00:00</published><updated>2025-12-05T00:00:00+00:00</updated><id>https://github.com/Wilson2022</id><content type="html" xml:base="https://github.com/Wilson2022/"><![CDATA[<p><strong>How does the Biological Carbon Pump change in future IPCC model simulations?</strong></p>

<blockquote>
  <p>Carbon storage by the Biological Carbon Pump consistently increases across the 21st century due to slowing circulation despite big uncertanties in the organic carbon flux to the deep ocean.</p>
</blockquote>]]></content><author><name>Jamie Wilson</name></author><category term="researchpaper" /><summary type="html"><![CDATA[How does the Biological Carbon Pump change in future IPCC model simulations?]]></summary></entry></feed>