{"id":849,"date":"2026-07-26T08:40:00","date_gmt":"2026-07-25T23:40:00","guid":{"rendered":"https:\/\/onepress.co.kr\/index.php\/briefing\/2026-07-26-net-zero-multicentury-cooling-en\/"},"modified":"2026-07-26T08:48:52","modified_gmt":"2026-07-25T23:48:52","slug":"2026-07-26-net-zero-multicentury-cooling-en","status":"publish","type":"briefing","link":"https:\/\/onepress.co.kr\/index.php\/briefing\/2026-07-26-net-zero-multicentury-cooling-en\/","title":{"rendered":"Centuries after net-zero GHG, a study finds at least 0.6 C of cooling"},"content":{"rendered":"<p><strong>2026-07-26 08:40 KST<\/strong><\/p>\n<p>Sustaining net-zero across multiple greenhouse gases could lower global mean temperature by at least 0.6 C over the following centuries, according to a new analysis.<\/p>\n<p>That does not mean stopping every emission today would cool Earth immediately. The result depends on continued net-negative CO2 removing enough carbon to offset residual methane, nitrous oxide, and other gases.<\/p>\n<h2>CO2 cessation is not net-zero GHG<\/h2>\n<p>The long-term temperature response after CO2 emissions stop is called the zero emissions commitment, or ZEC. Using three constrained climate metrics, the study estimated a near-zero multi-century ZEC for historical CO2 emissions.<\/p>\n<p>Real net-zero GHG policy is different. Residual methane and nitrous oxide are balanced with CO2 removal, so CO2 itself can remain net-negative even when the aggregate is zero.<\/p>\n<h2>Why at least 0.6 C of cooling appears<\/h2>\n<p>The authors call the policy-relevant effect Net-ZEC. Across scenarios and greenhouse-gas offsetting conventions, it produced at least 0.6 C of multi-century cooling after net-zero GHG.<\/p>\n<p>The driver is continued net CO2 removal used to offset residual non-CO2 gases. Net-zero is therefore a state that must be maintained, not a date that ends the work.<\/p>\n<figure class=\"wp-block-image size-full\"><img decoding=\"async\" src=\"https:\/\/onepress.co.kr\/wp-content\/uploads\/2026\/07\/net-zero-multicentury-cooling-en.png\" alt=\"Produced image explaining residual greenhouse gases, sustained carbon removal, and slow multi-century cooling after net-zero GHG\" loading=\"lazy\" \/><figcaption class=\"op-briefing-image-caption\">Produced image: ONEPRESS illustrates sustained net-zero greenhouse gases, residual-emissions offsetting, and multi-century temperature change. It is not a photograph of a specific future scenario.<\/figcaption><\/figure>\n<h2>How this changes the simple picture<\/h2>\n<p>The physical statement that temperature roughly stabilizes after CO2 cessation is not the same as sustaining net-zero across a mixture of gases. The IPCC also says sustained net-zero GHG is projected to bring a gradual decline after peak temperature and implies net-negative CO2.<\/p>\n<p>The new study separates and quantifies these two ideas.<\/p>\n<h2>Do not read 0.6 C as a short-term forecast<\/h2>\n<p>The result unfolds over centuries and depends on simplified climate models, existing multi-model data, policy scenarios, greenhouse-gas metrics, and sustained removal. It does not mean heatwaves or extreme rainfall disappear quickly.<\/p>\n<p>Sea level, ocean heat, and ice sheets also do not reverse at the same rate as surface temperature.<\/p>\n<h2>The policy has to persist<\/h2>\n<p>Cooling occurs only if net-zero GHG and net-negative CO2 removal are maintained for the long term. A change in residual emissions or removal changes the path. More complex Earth-system model tests are the next important check.<\/p>\n<h2>Official Primary Sources<\/h2>\n<p><a href=\"https:\/\/www.nature.com\/articles\/s41558-026-02700-2\" target=\"_blank\" rel=\"noopener noreferrer\">Nature Climate Change original study<\/a><\/p>\n<p><a href=\"https:\/\/doi.org\/10.5281\/zenodo.10120439\" target=\"_blank\" rel=\"noopener noreferrer\">Zenodo research data and code<\/a><\/p>\n<p><a href=\"https:\/\/www.ipcc.ch\/report\/ar6\/syr\/summary-for-policymakers\/\" target=\"_blank\" rel=\"noopener noreferrer\">IPCC AR6 Synthesis Report Summary for Policymakers<\/a><\/p>\n<p><a href=\"https:\/\/eartharxiv.org\/repository\/view\/9100\/\" target=\"_blank\" rel=\"noopener noreferrer\">EarthArXiv author preprint<\/a><\/p>\n","protected":false},"excerpt":{"rendered":"<p>Sustaining net-zero across multiple greenhouse gases could lower global mean temperature by at least 0.6 C over centuries. This is not immediate cooling from stopping all emissions today; it depends on continued net-negative CO2 offsetting residual gases.<\/p>\n","protected":false},"featured_media":0,"template":"","meta":[],"class_list":["post-849","briefing","type-briefing","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/onepress.co.kr\/index.php\/wp-json\/wp\/v2\/briefing\/849","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/onepress.co.kr\/index.php\/wp-json\/wp\/v2\/briefing"}],"about":[{"href":"https:\/\/onepress.co.kr\/index.php\/wp-json\/wp\/v2\/types\/briefing"}],"wp:attachment":[{"href":"https:\/\/onepress.co.kr\/index.php\/wp-json\/wp\/v2\/media?parent=849"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}