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		<title>Dust and clouds reshape how Earth cools when the Atlantic circulation slows</title>
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		<pubDate>Fri, 23 Oct 2026 20:37:00 +0000</pubDate>
				<category><![CDATA[Chemistry]]></category>
		<category><![CDATA[aerosol-cloud interactions]]></category>
		<category><![CDATA[AMOC]]></category>
		<category><![CDATA[climate modelling]]></category>
		<category><![CDATA[freshwater hosing]]></category>
		<category><![CDATA[ice-nucleating particles]]></category>
		<category><![CDATA[ICON-HAM]]></category>
		<category><![CDATA[ITCZ]]></category>
		<category><![CDATA[mixed-phase clouds]]></category>
		<category><![CDATA[North Atlantic]]></category>
		<category><![CDATA[radiative forcing]]></category>
		<category><![CDATA[Saharan dust]]></category>
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					<description><![CDATA[A model study finds that a 60 percent weakening of the Atlantic overturning circulation raises Northern Hemisphere aerosol loads by 41 percent, mostly through enhanced Saharan dust and longer particle lifetimes, reshaping clouds and adding to the cooling response.]]></description>
		
		
		
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