{"id":3501410,"date":"2024-05-29T08:01:00","date_gmt":"2024-05-29T08:01:00","guid":{"rendered":"https:\/\/www.resilience.org\/?p=3501410"},"modified":"2024-06-19T18:59:11","modified_gmt":"2024-06-19T18:59:11","slug":"navigating-climate-catastrophe-part-2-the-response","status":"publish","type":"post","link":"https:\/\/www.resilience.org\/stories\/2024-05-29\/navigating-climate-catastrophe-part-2-the-response\/","title":{"rendered":"Navigating Climate Catastrophe: Part 2 \u2013 The Response"},"content":{"rendered":"<p><i><span style=\"font-weight: 400;\">This is Part 2 of an exploration of the current state of the climate crisis. Please read <a href=\"\/stories\/2024-05-28\/navigating-climate-catastrophe-part-1-the-predicament\/\">Part\u00a01<\/a> first.<\/span><\/i><\/p><p><b>What to Expect<\/b><\/p><p><span style=\"font-weight: 400;\">Because climate change is complicated and climate science is incomplete, it\u2019s hard to predict exactly what will happen this century as a result of global warming. But we have some clues.<\/span><\/p><p><span style=\"font-weight: 400;\">There\u2019s no precedent for catastrophic climate change during human history (the most impactful climate shift for which we have documentation was perhaps the <\/span><a href=\"https:\/\/www.newyorker.com\/magazine\/2019\/04\/01\/how-the-little-ice-age-changed-history\"><span style=\"font-weight: 400;\">Little Ice Age<\/span><\/a><span style=\"font-weight: 400;\"> of the 14<\/span><span style=\"font-weight: 400;\">th<\/span><span style=\"font-weight: 400;\"> to the 19<\/span><span style=\"font-weight: 400;\">th<\/span><span style=\"font-weight: 400;\"> centuries\u2014though it was only regional, mainly affecting Europe). But, over geologic time, there is one instance that\u2019s analogous. About 56 million years ago, natural processes produced warming that was greatly worsened by climate feedbacks. The Earth\u2019s average surface temperature increased by 7 degrees Celsius. This event is known to geologists as the Paleocene Eocene Thermal Maximum (PETM).\u00a0<\/span><\/p><p><span style=\"font-weight: 400;\">The PETM was a <\/span><a href=\"https:\/\/www.climate.gov\/teaching\/resources\/petm-unearthing-ancient-climate-change-21273\"><span style=\"font-weight: 400;\">big deal<\/span><\/a><span style=\"font-weight: 400;\">. Triggered probably by volcanoes in the North Atlantic coinciding with a warming phase of the <\/span><a href=\"https:\/\/science.nasa.gov\/science-research\/earth-science\/milankovitch-orbital-cycles-and-their-role-in-earths-climate\/\"><span style=\"font-weight: 400;\">Milankovitch Cycle<\/span><\/a><span style=\"font-weight: 400;\">, the warming pulse was amplified by the release of methane from melting permafrost and methane hydrates. Surprisingly few creatures went extinct, but ones that survived were forced to migrate long distances. The oceans became acidic and were depleted of oxygen. Land vegetation shifted toward the poles. The warming and its immediate effects persisted for 180,000 years.<\/span><\/p><p><span style=\"font-weight: 400;\">For us in the 21<\/span><span style=\"font-weight: 400;\">st<\/span><span style=\"font-weight: 400;\"> century, this may represent a worst-case scenario. Good news: feedbacks that made the PETM so catastrophic haven\u2019t kicked in yet. Bad news: the climate forcing we\u2019re doing is of nearly as great a magnitude, and at a much greater speed.<\/span><\/p><div class=\"resp-content-preview-message\">\r\n\t<h2>See more at Resilience+<\/h2>\r\n\t<p>Log in&mdash;or sign up for free&mdash;to see the rest of this post at Resilience+, where you can get first-hand access to events with experts, facilitated discussions, and educational resources.<\/p>\r\n\t<a class=\"res-btn-yellow\" href=\"\/enter\/\">Log In or Sign Up<\/a>\r\n\t<\/div>","protected":false},"excerpt":{"rendered":"<p>People have all sorts of different interpretations on what\u2019s happening with climate change. While some are practicing denial or willful ignorance, even those following the science can be confused. After all, Earth\u2019s climate system is complex. In Part 2, Richard Heinberg unpacks some recent research on the likely consequences of global warming this century and beyond and recommends practical things we can do to both mitigate and adapt to the consequences. (See <a href=\"\/stories\/2024-05-28\/navigating-climate-catastrophe-part-1-the-predicament\/\">part 1<\/a>, in case you missed it.)<\/p>\n","protected":false},"author":128248,"featured_media":3501407,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[252007],"tags":[],"class_list":["post-3501410","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-resilience-plus"],"acf":[],"_links":{"self":[{"href":"https:\/\/www.resilience.org\/wp-json\/wp\/v2\/posts\/3501410","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.resilience.org\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.resilience.org\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.resilience.org\/wp-json\/wp\/v2\/users\/128248"}],"replies":[{"embeddable":true,"href":"https:\/\/www.resilience.org\/wp-json\/wp\/v2\/comments?post=3501410"}],"version-history":[{"count":0,"href":"https:\/\/www.resilience.org\/wp-json\/wp\/v2\/posts\/3501410\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/www.resilience.org\/wp-json\/wp\/v2\/media\/3501407"}],"wp:attachment":[{"href":"https:\/\/www.resilience.org\/wp-json\/wp\/v2\/media?parent=3501410"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.resilience.org\/wp-json\/wp\/v2\/categories?post=3501410"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.resilience.org\/wp-json\/wp\/v2\/tags?post=3501410"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}