{"id":166913,"date":"2020-08-17T12:00:32","date_gmt":"2020-08-17T11:00:32","guid":{"rendered":"https:\/\/www.transcend.org\/tms\/?p=166913"},"modified":"2020-08-16T15:04:03","modified_gmt":"2020-08-16T14:04:03","slug":"are-worst-case-climate-scenarios-less-likely-as-media-reports-of-a-new-scientific-paper-suggest","status":"publish","type":"post","link":"https:\/\/www.transcend.org\/tms\/2020\/08\/are-worst-case-climate-scenarios-less-likely-as-media-reports-of-a-new-scientific-paper-suggest\/","title":{"rendered":"Are Worst-Case Climate Scenarios Less Likely, as Media Reports of a New Scientific Paper Suggest?"},"content":{"rendered":"<p><em>28 Jul 2020 &#8211; <\/em>Reading the media reporting of a new scientific paper released on 22 July, it was easy to get the impression that some \u201cworse-case\u201d climate warming possibilities are now off the agenda. \u201cSo this is good news?\u201d a friend emailed. \u201cNo\u201d was my answer.<\/p>\n<p>It would be a grave mistake, and an illustration of how media reporting can get complex climate stories wrong, to find good news in this research.<\/p>\n<p><em><a href=\"https:\/\/www.transcend.org\/tms\/wp-content\/uploads\/2020\/08\/climate-environ.jpg\" ><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-166915\" src=\"https:\/\/www.transcend.org\/tms\/wp-content\/uploads\/2020\/08\/climate-environ.jpg\" alt=\"\" width=\"400\" height=\"304\" srcset=\"https:\/\/www.transcend.org\/tms\/wp-content\/uploads\/2020\/08\/climate-environ.jpg 400w, https:\/\/www.transcend.org\/tms\/wp-content\/uploads\/2020\/08\/climate-environ-300x228.jpg 300w\" sizes=\"auto, (max-width: 400px) 100vw, 400px\" \/><\/a><\/em><\/p>\n<p>The research in question is <a href=\"https:\/\/agupubs.onlinelibrary.wiley.com\/doi\/abs\/10.1029\/2019RG000678\"  target=\"_blank\" rel=\"noopener noreferrer\">\u201cAn assessment of Earth\u2019s climate sensitivity using multiple lines of evidence\u201d<\/a>. Climate sensitivity is the amount of warming to be expected from a doubling of the amount of carbon dioxide in the atmosphere. The most recent Intergovernmental Panel on Climate Change (IPCC) report found the range was 1.5 to 4.5 degrees Celsius (\u00b0C).<\/p>\n<p>The new paper uses multiple lines of evidence \u2014 observations over the last 150 years, climate models, and climate history reaching back almost four million years \u2014 to constrain the estimated range for climate sensitivity.<\/p>\n<div>One major finding was that very low estimates of climate sensitivity of less than 2\u00b0C \u2014 which climate sceptics like to emphasise \u2014 are inconsistent with the evidence. The <a href=\"https:\/\/www.washingtonpost.com\/weather\/2020\/07\/22\/climate-sensitivity-co2\/\"  target=\"_blank\" rel=\"noopener noreferrer\">Washington Post headlined<\/a> with \u201cMajor new climate study rules out less severe global warming scenarios\u201d, reporting that the research \u201cfound that Earth\u2019s global average temperature will most likely increase between 2.3 and 4.5\u00b0C\u201d compared to the IPCC range of 1.5-4.5\u00b0C. And it reported that there \u201cwould be a 6 to 18 percent chance of exceeding the upper bound defined by the study 4.5\u00b0C.\u201d Which was balanced reporting.<\/div>\n<div><\/div>\n<div>Other coverage gave emphasis to the claim that some high-end estimates might now be off the table. But if the IPCC range was up 4.5\u00b0C, and the new paper range is up 4.5\u00b0C, what has changed that is \u201cgood news\u201d?\u00a0 Some research papers over the last two years, reporting on preliminary results from updated climate models for the next IPCC report, had suggested that climate sensitivity could be much higher, due to unresolved issues with cloud feedbacks. But scientists such as NASA\u2019S Gavin Schmidt had <a href=\"http:\/\/www.realclimate.org\/index.php\/archives\/2020\/06\/sensitive-but-unclassified-part-ii\/\"  target=\"_blank\" rel=\"noopener noreferrer\">warned<\/a> that this work-in-progess should be taken with a grain of salt: \u201cclaims that climate sensitivity is much higher, or that worst cases scenarios need to be revised upwards, are premature\u201d.\u00a0 His warning was prescient.<\/div>\n<p>And <a href=\"https:\/\/www.sciencedaily.com\/releases\/2020\/07\/200722112648.htm\"  target=\"_blank\" rel=\"noopener noreferrer\">Science Daily reported<\/a> one of the paper&#8217;s authors, Gabi Hegerl, saying that \u201cthese estimates make it improbable that climate sensitivity is at the low end of the IPCC range and <b>confirm the upper range<\/b>\u201d (emphasis added).<\/p>\n<p>Even though the new paper had found the upper bound of 4.5\u00b0C was the same as that of the IPCC report, media reporting included: <em><br \/>\n<\/em><\/p>\n<ul>\n<li>\u201cIt presents both good and bad news. The worst-case climate scenarios may be somewhat less likely than previous studies suggested. But the best-case climate scenarios \u2014 those assuming the least amount of warming \u2014 are almost certainly not going to happen\u201d, <a href=\"https:\/\/www.blogger.com\/%E2%80%A8https:\/\/www.eenews.net\/stories\/1063611707\"  target=\"_blank\" rel=\"noopener noreferrer\">reported E&amp;E News<\/a>.<\/li>\n<li><a href=\"https:\/\/www.carbonbrief.org\/guest-post-why-low-end-climate-sensitivity-can-now-be-ruled-out\"  target=\"_blank\" rel=\"noopener noreferrer\">Carbon Brief reported<\/a> that \u201cthe silver lining to this cloud is that our findings also suggest that very high Equilibrium Climate Sensitivity (ECS &#8211; see below) estimates are unlikely\u201d.<\/li>\n<li><a href=\"https:\/\/theconversation.com\/the-climate-wont-warm-as-much-as-we-feared-but-it-will-warm-more-than-we-hoped-143175\"  target=\"_blank\" rel=\"noopener noreferrer\">The Conversation headlined<\/a> with \u201cThe climate won\u2019t warm as much as we feared \u2013 but it will warm more than we hoped\u201d; at arsTechnica, it was \u201cMajor study rules out super-high and low climate sensitivity to CO2\u201d.<\/li>\n<\/ul>\n<p>The impression across this reporting was that some of the more high-end warming estimates are now off the table. So should we be comforted that \u201cour findings also suggest that very high ECS estimates are unlikely\u201d or that \u201cthe climate won\u2019t warm as much as we feared\u201d?<\/p>\n<p>What none of the media reports said \u2014 as far as I can ascertain \u2014 is that this new study is only about short-term warming, not the \u201cslow\u201d warming where the full impacts of climate change on ice sheets and carbon stores are taken into account. And that leads to a very different story.<\/p>\n<p><b>Two types of climate sensitivity<\/b><\/p>\n<p>Climate sensitivity is generally understood as the temperature rise subsequent to a doubling of the level of carbon dioxide (CO2), once the planetary system has returned to equilibrium (balance); that is, once all the perturbations caused by the increase in trapped energy have worked their way through the system, including hotter atmosphere and oceans, melting ice sheets, changed vegetation and so on. Whilst some of the impacts are fast and can be observed on short to decadal timeframes (atmospheric warming, changes to clouds, increased water vapour), others such as the melting of the polar ice sheets or large-scale loss of frozen carbon stores (permafrost) are more relevant on century to millenia timeframes. These \u201cslow\u201d feedbacks (self-reinforcing loops) can take many human generations in time to manifest.<\/p>\n<p>IPCC reports have focused on what is generally called <b>Equilibrium Climate Sensitivity <\/b>(ECS).\u00a0 The 2007 IPCC report gave a best estimate of climate sensitivity of 3\u00b0C and says it \u201cis likely to be in the range 2\u00b0C to 4.5\u00b0C\u201d. The 2014 report said that \u201cno best estimate for equilibrium climate sensitivity can now be given because of a lack of agreement on values across assessed lines of evidence and studies\u201d and only gives a range of 1.5\u00b0C to 4.5\u00b0C.<\/p>\n<p>What the IPCC reports failed to make clear is that the ECS measure omits key &#8220;slow&#8221; feedbacks that a rise in the planet&#8217;s temperature can trigger. These include the permafrost feedback and other changes in the carbon cycle which can release large amounts of greenhouse gases to the atmosphere, a decrease in the ocean&#8217;s carbon-sink efficiency, and the melting of polar ice sheets and hence changes in the Earth&#8217;s reflectivity.<em><br \/>\n<\/em><\/p>\n<div>Climate sensitivity which includes these feedbacks\u00a0 \u2014 known as <b>Earth System Sensitivity<\/b> (ESS) \u2014 does not appear to be acknowledged in the 2014 IPCC report at all. Yet, there is a wide range of literature which suggest an ESS of 5\u20136\u00b0C, for example by the <a href=\"https:\/\/www.geolsoc.org.uk\/~\/media\/shared\/documents\/policy\/Statements\/Climate%20Change%20Statement%20Addendum%202013%20Final.pdf\"  target=\"_blank\" rel=\"noopener noreferrer\">Geological Society<\/a> and a lifetime of work by former NASA climate science chief James Hansen and his co-researchers, including <a href=\"https:\/\/royalsocietypublishing.org\/doi\/full\/10.1098\/rsta.2012.0294\"  target=\"_blank\" rel=\"noopener noreferrer\">&#8220;Climate sensitivity, sea level and atmospheric carbon dioxide&#8221;<\/a>.<\/div>\n<div><\/div>\n<div><\/div>\n<div><a target=\"_blank\" href=\"https:\/\/1.bp.blogspot.com\/-dLTY6b562bQ\/Xx9t4k0I10I\/AAAAAAAAAco\/tHVJkPPcicsebpzl7dlGdn7Ye0tJzt-igCLcBGAsYHQ\/s923\/800000%2Byears%2Bpaleo.jpg\" ><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter\" src=\"https:\/\/1.bp.blogspot.com\/-dLTY6b562bQ\/Xx9t4k0I10I\/AAAAAAAAAco\/tHVJkPPcicsebpzl7dlGdn7Ye0tJzt-igCLcBGAsYHQ\/w400-h253\/800000%2Byears%2Bpaleo.jpg\" width=\"400\" height=\"253\" border=\"0\" data-original-height=\"582\" data-original-width=\"923\" \/><\/a><\/div>\n<div><\/div>\n<div><\/div>\n<div>The long-term (slow feedbacks) or <b>Earth System Sensitivity<\/b> can be inferred from the paleoclimate record. Over the last million years, the Earth\u2019s climate has see-sawed between atmospheric CO2 of around 180 parts per million (ppm) in glacial periods and 300 ppm CO2 during interglacial or warm periods (see illustration, drawn from the Hansen et al paper referenced above). This is an increase in CO2 levels of around 65%, that is, less than a doubling.\u00a0 Yet during such periods, the temperature see-sawed by up to 5\u00b0C. Now, there are some other factors to take into account that have an influence in triggering this process, principally changes in Earth\u2019s orbit (Milankovitch cycles). Nevertheless there is a wide range of recent literature that points to ESS of around 5-6\u00b0C, such as <a href=\"https:\/\/www.pnas.org\/content\/114\/39\/10315\"  target=\"_blank\" rel=\"noopener noreferrer\">\u201cWell below 2C: Mitigation strategies for avoiding dangerous to catastrophic climate changes\u201d<\/a>.<\/div>\n<p>So does the recent climate sensitivity paper deal with Equilibrium Climate Sensitivity (fast feedbacks only) or Earth System Sensitivity (including slow feedbacks)? The evidence is clear that it does not include slow feedbacks.\u00a0 For example:<em><br \/>\n<\/em><\/p>\n<ul>\n<li>The paper notes that Earth\u2019s Equilibrium Climate Sensitivity (ECS) is defined generally as \u201cthe steady-state global\u00a0 temperature increase for a doubling of CO2, has long been taken as the starting point for\u00a0 understanding global climate changes. It was quantified specifically by Charney et al. as the equilibrium warming as seen in a model <b>with ice sheets and vegetation fixed at present-day values<\/b>\u201d (emphasis added).\u00a0 In other words, slow feedbacks are excluded.<\/li>\n<li>The paper uses a term <b><i>S<\/i><\/b> to denote \u201ceffective climate sensitivity\u201d, which is derived from the traditional ECS definition, but based on the impacts at 150 years after an increase in CO2 levels, rather than the longer period in which equilibrium has been restored. The paper notes that it \u201cdoes not formally exclude any feedback process, but <b>the 150-year time frame minimizes slow feedbacks (especially ice sheet changes)<\/b>\u201d\u00a0 (emphasis added), and \u201cOur <b><i>S<\/i><\/b> incorporates only feedbacks acting on time scales of order a century\u201d.\u00a0 Given that slow feedbacks generally are relevant on longer than century timescales, it is again clear that they are not included.<\/li>\n<li>And <b><i>S<\/i><\/b> is compared with \u201cEarth System Sensitivity, (which) <b>by contrast, reflects the slower feedback processes such as changes to the carbon cycle and land ice<\/b>\u201d (emphasis added).<\/li>\n<li>And again: \u201cIn this assessment we consider well-mixed gases (CO2, CH4, N2O) to be specified forcers, since in the modern era, they are effectively under human control. Thus <b>we do not include climate-driven variations of these gases (e.g., carbon cycle feedbacks)\u201d (emphasis added).\u2028<\/b><\/li>\n<li><b>In fact, in that section of the paper using data from climate history <\/b>back millions of years, the role of slow feedbacks are excluded in order to gain insight into the role of fast feedbacks only: \u201cThe paleoclimate data come from intervals where the climate was different to today, but fairly stable for several thousand years, meaning that slow feedback processes need to be taken into account. By treating these slow processes as forcings rather than feedbacks, we are able to make inferences about <b><i>S<\/i><\/b>. Both the temperature changes that are used, <b>and the slow feedback influences that are removed<\/b>, are constrained using indirect proxy records\u201d (emphasis added).<\/li>\n<\/ul>\n<div><\/div>\n<div><b>Consequences<\/b><\/div>\n<div><\/div>\n<div>So what does all this mean?<\/div>\n<ol>\n<li>The new paper has not reduced the higher end of the range for short-term sensitivity; in fact it has reaffirmed the 4.5\u00b0C boundary from the most recent IPCC assessment report.<\/li>\n<li>The paper under discussion is concerned with climate sensitivity including fast feedbacks only (Equilibrium Climate Sensitivity), so it has nothing new to say about the eventual warming caused by increased levels of greenhouse gases once slow feedbacks are taken into account (Earth System Sensitivity).<\/li>\n<li>The estimates of Earth System Sensitivity including slow feedbacks remain unaffected, which are likely in the 5-6\u00b0C range.<\/li>\n<li>Using that sensitivity, just the present level of CO2 of 415ppm, if maintained, would be enough with the slow feedbacks to eventually increase the global average temperature by 2.8-3.2\u00b0C. This would be a <a target=\"_blank\" href=\"http:\/\/www.climatecodered.org\/2020\/02\/a-climate-reality-update-at-2020.html%E2%80%A8\" >catastrophic level of warming<\/a>, including sea-level rises in the tens of metres, and swathes of the planet too hot for human habitation. This is consistent with the paleoclimate record of past climates, for example, <a href=\"https:\/\/www.nature.com\/articles\/s41598-020-67154-8%E2%80%A8\"  target=\"_blank\" rel=\"noopener noreferrer\">here<\/a> and <a href=\"https:\/\/www.nature.com\/articles\/ngeo724%E2%80%A8\"  target=\"_blank\" rel=\"noopener noreferrer\">here<\/a> and <a href=\"https:\/\/www.pnas.org\/content\/115\/52\/13288%E2%80%A8\"  target=\"_blank\" rel=\"noopener noreferrer\">here<\/a> and <a href=\"http:\/\/www.columbia.edu\/~jeh1\/mailings\/2018\/20181019_FromXianWithLove.pdf%E2%80%A8\"  target=\"_blank\" rel=\"noopener noreferrer\">here<\/a>.\u2028 By contrast, using the ECS measure of 3\u00baC, the resulting warming would be 1.7\u00b0C, around half a degree hotter than now, so understanding what climate sensitivity assumptions are behind a future warming projection is important!<\/li>\n<li>Whilst \u201cslow feedbacks\u201d such as the \u201crelease of greenhouse gases from thawing permafrost, reduced ocean and terrestrial CO2 removal from the atmosphere\u201d are generally considered to operate on slow timescales, a <a href=\"https:\/\/www.csis.org\/analysis\/age-consequences%E2%80%A8\"  target=\"_blank\" rel=\"noopener noreferrer\">report<\/a> as far back as 2007 was able to conclude \u201cthere is some evidence that such feedbacks may already be occurring in response to the present warming trend\u201d because the rate of warming driven by human actions is faster than at any time in the past.\u00a0 In fact if we look at more recent evidence from the polar regions, it is clear that the <a href=\"https:\/\/www.arctic.noaa.gov\/Report-Card%E2%80%A8\"  target=\"_blank\" rel=\"noopener noreferrer\">permafrost feedback<\/a> is already non-negligible, and that both <a href=\"https:\/\/www.nature.com\/articles\/s41586-019-1855-2%E2%80%A8\"  target=\"_blank\" rel=\"noopener noreferrer\">Greenland<\/a> and the <a href=\"https:\/\/www.nasa.gov\/press-release\/ramp-up-in-antarctic-ice-loss-speeds-sea-level-rise\"  target=\"_blank\" rel=\"noopener noreferrer\">Antarctic ice sheet<\/a> are exhibiting increasing rates of ice mass loss.<\/li>\n<li>In other words, warming of well less than 2\u00b0C can trigger slow feedbacks. In a personal communication on 19 March 2018, James Hansen told me that: &#8220;Global temperature has risen well out of the Holocene range and Earth is now as warm as it was during the prior (Eemian) interglacial period, when sea level reached 6-9 meters higher than today. Limiting the period and magnitude of temperature excursion above the Holocene range is crucial to avoid strong stimulation of slow feedbacks. A danger of 1.5\u00b0C or 2\u00b0C targets is that they are far above the Holocene temperature range. A long-term global average temperature of even 1.5\u00b0C could spur \u2018slow\u2019 climate feedbacks and is not an appropriate goal.\u201d<\/li>\n<\/ol>\n<p>And that is a story that the media coverage of this important new paper failed to tell.<\/p>\n<p><a target=\"_blank\" href=\"http:\/\/www.climatecodered.org\/2020\/07\/are-worst-case-climate-scenarios-less.html\" >Go to Original &#8211; climatecodered.com<\/a><\/p>\n","protected":false},"excerpt":{"rendered":"<p>28 Jul 2020 &#8211; Reading the media reporting of a new scientific paper released on 22 July, it was easy to get the impression that some \u201cworse-case\u201d climate warming possibilities are now off the agenda. \u201cSo this is good news?\u201d a friend emailed. \u201cNo\u201d was my answer. It would be a grave mistake, and an illustration of how media reporting can get complex climate stories wrong, to find good news in this research.\u00a0<\/p>\n","protected":false},"author":4,"featured_media":166915,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[61],"tags":[686,401,993],"class_list":["post-166913","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-environment","tag-climate-change","tag-environment","tag-global-warming"],"_links":{"self":[{"href":"https:\/\/www.transcend.org\/tms\/wp-json\/wp\/v2\/posts\/166913","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.transcend.org\/tms\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.transcend.org\/tms\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.transcend.org\/tms\/wp-json\/wp\/v2\/users\/4"}],"replies":[{"embeddable":true,"href":"https:\/\/www.transcend.org\/tms\/wp-json\/wp\/v2\/comments?post=166913"}],"version-history":[{"count":0,"href":"https:\/\/www.transcend.org\/tms\/wp-json\/wp\/v2\/posts\/166913\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/www.transcend.org\/tms\/wp-json\/wp\/v2\/media\/166915"}],"wp:attachment":[{"href":"https:\/\/www.transcend.org\/tms\/wp-json\/wp\/v2\/media?parent=166913"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.transcend.org\/tms\/wp-json\/wp\/v2\/categories?post=166913"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.transcend.org\/tms\/wp-json\/wp\/v2\/tags?post=166913"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}