<?xml version="1.0" encoding="UTF-8"?><rss xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:content="http://purl.org/rss/1.0/modules/content/" xmlns:atom="http://www.w3.org/2005/Atom" version="2.0"><channel><title><![CDATA[Climate models show considerable discrepancies in their future projections around the Atlantic, mainly due to uncertainties in the fate of the Atlantic Meridional Overturning Circulation (#AMOC).]]></title><description><![CDATA[<p>Climate models show considerable discrepancies in their future projections around the Atlantic, mainly due to uncertainties in the fate of the Atlantic Meridional Overturning Circulation (<a href="https://scicomm.xyz/tags/AMOC" rel="tag">#<span>AMOC</span></a>).</p><p><a href="https://scicomm.xyz/tags/Climate" rel="tag">#<span>Climate</span></a> models have previously suggested a reduction in AMOC strength of 32±37% by 2100.</p><p>But a closer examination, however, gives an estimate of the AMOC slowdown of 51±8%.</p><p>This refinement mainly results from correcting a bias in South Atlantic surface <a href="https://scicomm.xyz/tags/salinity" rel="tag">#<span>salinity</span></a>, consistent with recent studies emphasizing its role in the proximity to an AMOC tipping point.</p><p>This more substantial AMOC weakening has key implications for future <a href="https://scicomm.xyz/tags/adaptation" rel="tag">#<span>adaptation</span></a> strategies.</p><p><div class="card col-md-9 col-lg-6 position-relative link-preview p-0">

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