{"id":6333,"date":"2023-05-22T22:00:00","date_gmt":"2023-05-22T22:00:00","guid":{"rendered":"https:\/\/modernsciences.org\/staging\/4414\/?p=6333"},"modified":"2023-05-12T18:50:03","modified_gmt":"2023-05-12T18:50:03","slug":"smoke-from-the-black-summer-fires-could-have-made-the-triple-la-nina-more-likely","status":"publish","type":"post","link":"https:\/\/modernsciences.org\/staging\/4414\/smoke-from-the-black-summer-fires-could-have-made-the-triple-la-nina-more-likely\/","title":{"rendered":"Smoke from the Black Summer fires could have made the triple La Ni\u00f1a more likely"},"content":{"rendered":"\n<span><a href=\"https:\/\/theconversation.com\/profiles\/martin-jucker-379172\" target=\"_blank\" rel=\"noopener\">Martin Jucker<\/a>, <em><a href=\"https:\/\/theconversation.com\/institutions\/unsw-sydney-1414\" target=\"_blank\" rel=\"noopener\">UNSW Sydney<\/a><\/em><\/span>\n\n<p>The 2019-2020 bushfire season was devastating. Vast areas of pristine forest burned, many for the first time in memory. By some estimates, a billion native animals died up and down Australia\u2019s east coast. Dozens of people died. <\/p>\n\n<p>While Sydney\u2019s skies are blue again, Australia\u2019s Black Summer has kept scientists around the globe busy. The sheer size of these megafires produced startling effects. Recently, researchers found the huge volumes of smoke <a href=\"https:\/\/www.abc.net.au\/news\/2023-03-10\/how-the-black-summer-bushfires-depleted-the-ozone-layer\/102076136\" target=\"_blank\" rel=\"noopener\">ate away<\/a> at our protective ozone layer. <\/p>\n\n<p>Now, <a href=\"https:\/\/dx.doi.org\/10.1126\/sciadv.adg1213\" target=\"_blank\" rel=\"noopener\">new research<\/a> by American scientists suggests the Black Summer fires were massive enough to influence the <a href=\"https:\/\/cosmosmagazine.com\/earth\/enso-iod-weather-patterns-explainer\/#:%7E:text=El%20Ni%C3%B1o%20and%20La%20Ni%C3%B1a%2C%20also%20called%20El%20Ni%C3%B1o%20Southern,to%20the%20north%20of%20Australia.\" target=\"_blank\" rel=\"noopener\">El Ni\u00f1o Southern Oscillation cycle<\/a>. It\u2019s one of the most important drivers of unusual weather over the entire globe \u2013\u00a0and one which Australians know intimately.<\/p>\n\n<p>The <a href=\"https:\/\/theconversation.com\/la-nina-is-finishing-an-extremely-unusual-three-year-cycle-heres-how-it-affected-weather-around-the-world-196561\" target=\"_blank\" rel=\"noopener\">three successive years<\/a> of La Ni\u00f1a we just had? They could have been made more likely by the Black Summer fires. The reason, strangely enough, is the smoke. <\/p>\n\n<p>But it\u2019s important not to say the link is proven. While groundbreaking, this research relies on a single model. It\u2019s too early to clearly say bushfire smoke can trigger La Ni\u00f1a. <\/p>\n\n\n\n<h2 id=\"where-theres-fire-theres-smoke\">Where there\u2019s fire, there\u2019s smoke<\/h2>\n\n<p>We\u2019ve long known that the huge volume of ash blown high into the upper atmosphere by a big volcanic eruption can cool Earth\u2019s surface for many months, or <a href=\"https:\/\/www.ipcc.ch\/report\/sixth-assessment-report-working-group-i\/\" target=\"_blank\" rel=\"noopener\">even years<\/a>. <\/p>\n\n<p>We also know volcanoes <a href=\"https:\/\/doi.org\/10.1007\/s41748-022-00331-z\" target=\"_blank\" rel=\"noopener\">can influence<\/a> the tropical Pacific, and thus affect whether an El Ni\u00f1o or a La Ni\u00f1a phase develops. <\/p>\n\n<p>How? By blocking light. Particles of ash reduce how much light gets to the surface. <\/p>\n\n<p>Volcanic ash gets blown high into the stratosphere, the part of the atmosphere just above the clouds where long-haul airplanes fly. Then, sunlight gets reflected before it reaches the ground, thus cooling the surface much like an umbrella can. <\/p>\n\n<h2 id=\"is-bushfire-smoke-the-same-as-volcanic-ash\">Is bushfire smoke the same as volcanic ash?<\/h2>\n\n<p>It\u2019s tempting to equate smoke with ash, and assume a large enough bushfire would have similar effects to a volcano. <\/p>\n\n<p>But there are important differences. Most obviously, a bushfire does not smell of rotten eggs.<\/p>\n\n<p>That might sound unimportant, but the rotten egg smell \u2013\u00a0which comes from sulfur \u2013 indicates major differences in the composition of volcanic ash and bushfire smoke. <\/p>\n\n<p>Different chemicals could mean very different responses to sunlight once in the atmosphere, which in turn could affect how much light is reflected. <\/p>\n\n<p>Second, bushfires don\u2019t explode.<\/p>\n\n<p>A decent volcano erupts with enough force to blast smoke high into the stratosphere. Bushfires don\u2019t have the same propulsive force.<\/p>\n\n<p>Bushfire smoke is hot, though, and hot smoke rises well. Some of the smoke from the Black Summer fires <a href=\"https:\/\/www.science.org\/doi\/abs\/10.1126\/science.abe1415\" target=\"_blank\" rel=\"noopener\">reached the stratosphere<\/a>, although after a much longer interval than for volcanic eruptions. <\/p>\n\n<p>So, does a large bushfire have the same effect on climate as a volcano?<\/p>\n\n<p>The American researchers begin by checking the similarities using climate model simulations. They found bushfire smoke does indeed shade the surface from sunlight in these simulations. <\/p>\n\n\n\n<p>How much? Over a region of the south-eastern Pacific, about 150 terawatts of sunlight bounced back to space \u2013 the equivalent of about 100,000 coal power plants. <\/p>\n\n<h2 id=\"clouds-matter\">Clouds matter<\/h2>\n\n<p>The surprising finding is how it happens. In contrast to eruptions, bushfire smoke didn\u2019t reflect the sunlight directly. Instead, clouds were responsible. <\/p>\n\n<p>How does that work? This is where the magic of the climate system kicks in. Our atmosphere, oceans and lands are constantly interacting with each other.<\/p>\n\n<figure class=\"align-center zoomable\">\n            <a href=\"https:\/\/images.theconversation.com\/files\/525315\/original\/file-20230510-17-634wtl.jpg?ixlib=rb-1.1.0&amp;q=45&amp;auto=format&amp;w=1000&amp;fit=clip\" target=\"_blank\" rel=\"noopener\"><img  decoding=\"async\"  alt=\"Clouds over ocean\"  src=\"data:image\/png;base64,iVBORw0KGgoAAAANSUhEUgAAAAEAAAABAQMAAAAl21bKAAAAA1BMVEUAAP+KeNJXAAAAAXRSTlMAQObYZgAAAAlwSFlzAAAOxAAADsQBlSsOGwAAAApJREFUCNdjYAAAAAIAAeIhvDMAAAAASUVORK5CYII=\"  class=\" pk-lazyload\"  data-pk-sizes=\"auto\"  data-ls-sizes=\"(min-width: 1466px) 754px, (max-width: 599px) 100vw, (min-width: 600px) 600px, 237px\"  data-pk-src=\"https:\/\/images.theconversation.com\/files\/525315\/original\/file-20230510-17-634wtl.jpg?ixlib=rb-1.1.0&amp;q=45&amp;auto=format&amp;w=754&amp;fit=clip\"  data-pk-srcset=\"https:\/\/images.theconversation.com\/files\/525315\/original\/file-20230510-17-634wtl.jpg?ixlib=rb-1.1.0&amp;q=45&amp;auto=format&amp;w=600&amp;h=401&amp;fit=crop&amp;dpr=1 600w, https:\/\/images.theconversation.com\/files\/525315\/original\/file-20230510-17-634wtl.jpg?ixlib=rb-1.1.0&amp;q=30&amp;auto=format&amp;w=600&amp;h=401&amp;fit=crop&amp;dpr=2 1200w, https:\/\/images.theconversation.com\/files\/525315\/original\/file-20230510-17-634wtl.jpg?ixlib=rb-1.1.0&amp;q=15&amp;auto=format&amp;w=600&amp;h=401&amp;fit=crop&amp;dpr=3 1800w, https:\/\/images.theconversation.com\/files\/525315\/original\/file-20230510-17-634wtl.jpg?ixlib=rb-1.1.0&amp;q=45&amp;auto=format&amp;w=754&amp;h=504&amp;fit=crop&amp;dpr=1 754w, https:\/\/images.theconversation.com\/files\/525315\/original\/file-20230510-17-634wtl.jpg?ixlib=rb-1.1.0&amp;q=30&amp;auto=format&amp;w=754&amp;h=504&amp;fit=crop&amp;dpr=2 1508w, https:\/\/images.theconversation.com\/files\/525315\/original\/file-20230510-17-634wtl.jpg?ixlib=rb-1.1.0&amp;q=15&amp;auto=format&amp;w=754&amp;h=504&amp;fit=crop&amp;dpr=3 2262w\" ><\/a>\n            <figcaption>\n              <span class=\"caption\">Whiter, thicker clouds make the surface of the ocean cooler.<\/span>\n              <span class=\"attribution\"><span class=\"source\">Shutterstock<\/span><\/span>\n            <\/figcaption>\n          <\/figure>\n\n<p>In their simulations, Black Summer smoke was first blown eastward by strong winds in the atmosphere. Under specific conditions, some smoke particles can interact with droplets in clouds and make clouds thicker and brighter. One region where this can happen is the subtropical south-eastern Pacific. <\/p>\n\n<p>The researchers were able to show the brightness of the clouds over this area increased considerably just around the time when the smoke particles arrived.  <\/p>\n\n<p>These brighter, whiter clouds reflected more sunlight back into space and shaded the surface underneath. The net effect: cooler seawater. <\/p>\n\n<p>The effect was particularly important because of the timing. Smoke-whitened clouds emerged around our summer solstice in late December, which is the same time of year when the strength of the incoming sunlight peaks in the southern hemisphere.<\/p>\n\n<p>How is this linked to La Ni\u00f1a? <\/p>\n\n<p>Follow the chain: huge volumes of smoke blow east where they whiten clouds, cool the seawater, and cause less water to evaporate.<\/p>\n\n<p>Surface winds carried this cooler, drier air over the tropical Pacific, where it cooled the ocean surface again, and made it harder for tropical storms to form.<\/p>\n\n<p>A cooler sea surface in the tropical Pacific is a hallmark of La Ni\u00f1a, the cold phase of the El Ni\u00f1o Southern Oscillation cycle. <\/p>\n\n<p>That\u2019s how this research was able to trace a link between Black Summer smoke and the rare back-to-back La Ni\u00f1a events in 2019-20 and 2020-21. As you know, we ended up having an even rarer triple La Ni\u00f1a in 2021-22, though the research period ends before this. <\/p>\n\n\n\n<h2 id=\"is-the-link-now-proven-not-quite\">Is the link now proven? Not quite<\/h2>\n\n<p>This study offers a consistent physical explanation for how bushfires might influence the El Ni\u00f1o cycle. <\/p>\n\n<p>It\u2019s yet another example of how complex climate science can be, and how much we can still be surprised and challenged by what mother nature presents us. <\/p>\n\n<p>But there are a few caveats to keep in mind.<\/p>\n\n<p>For one, the ENSO cycle in the simulation was heading for a double La Ni\u00f1a even without the impact of the smoke. The simulation stops in the winter of 2021, which is before the real-world ENSO tipped into a third La Ni\u00f1a. <\/p>\n\n<p>What does that mean? In short, we can\u2019t know for sure if the effect of the bushfire smoke really did cause the triple La Ni\u00f1a. <\/p>\n\n<p>Another caveat is the fact the study relied on a single climate model, and relies heavily on the representation of clouds in that model.<\/p>\n\n<p>That\u2019s a potential problem, because we know clouds \u2013 and especially their interactions with aerosols like smoke \u2013\u00a0are still the largest source of uncertainties and model errors. <\/p>\n\n<p>To prove or disprove the link, we\u2019ll have to simulate the impact of ballooning Black Summer smoke plumes across many different models. <!-- Below is The Conversation's page counter tag. Please DO NOT REMOVE. --><img  loading=\"lazy\"  decoding=\"async\"  src=\"data:image\/png;base64,iVBORw0KGgoAAAANSUhEUgAAAAEAAAABAQMAAAAl21bKAAAAA1BMVEUAAP+KeNJXAAAAAXRSTlMAQObYZgAAAAlwSFlzAAAOxAAADsQBlSsOGwAAAApJREFUCNdjYAAAAAIAAeIhvDMAAAAASUVORK5CYII=\"  alt=\"The Conversation\"  width=\"1\"  height=\"1\"  style=\"border: none !important; box-shadow: none !important; margin: 0 !important; max-height: 1px !important; max-width: 1px !important; min-height: 1px !important; min-width: 1px !important; opacity: 0 !important; outline: none !important; padding: 0 !important\"  referrerpolicy=\"no-referrer-when-downgrade\"  class=\" pk-lazyload\"  data-pk-sizes=\"auto\"  data-pk-src=\"https:\/\/counter.theconversation.com\/content\/205292\/count.gif?distributor=republish-lightbox-basic\" ><!-- End of code. If you don't see any code above, please get new code from the Advanced tab after you click the republish button. The page counter does not collect any personal data. More info: https:\/\/theconversation.com\/republishing-guidelines --><\/p>\n\n\n\n<p><span><a href=\"https:\/\/theconversation.com\/profiles\/martin-jucker-379172\" target=\"_blank\" rel=\"noopener\">Martin Jucker<\/a>, Lecturer in Atmospheric Dynamics, <em><a href=\"https:\/\/theconversation.com\/institutions\/unsw-sydney-1414\" target=\"_blank\" rel=\"noopener\">UNSW Sydney<\/a><\/em><\/span><\/p>\n\n<p>This article is republished from <a href=\"https:\/\/theconversation.com\" target=\"_blank\" rel=\"noopener\">The Conversation<\/a> under a Creative Commons license. Read the <a href=\"https:\/\/theconversation.com\/smoke-from-the-black-summer-fires-could-have-made-the-triple-la-nina-more-likely-205292\" target=\"_blank\" rel=\"noopener\">original article<\/a>.<\/p>\n\n","protected":false},"excerpt":{"rendered":"Martin Jucker, UNSW Sydney The 2019-2020 bushfire season was devastating. Vast areas of pristine forest burned, many for&hellip;\n","protected":false},"author":462,"featured_media":6325,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"nf_dc_page":"","fifu_image_url":"","fifu_image_alt":"","footnotes":""},"categories":[13],"tags":[141,580,704,474],"class_list":{"0":"post-6333","1":"post","2":"type-post","3":"status-publish","4":"format-standard","5":"has-post-thumbnail","7":"category-earth","8":"tag-australia","9":"tag-el-nino","10":"tag-la-nina","11":"tag-the-conversation","12":"cs-entry","13":"cs-video-wrap"},"aioseo_notices":[],"_links":{"self":[{"href":"https:\/\/modernsciences.org\/staging\/4414\/wp-json\/wp\/v2\/posts\/6333","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/modernsciences.org\/staging\/4414\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/modernsciences.org\/staging\/4414\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/modernsciences.org\/staging\/4414\/wp-json\/wp\/v2\/users\/462"}],"replies":[{"embeddable":true,"href":"https:\/\/modernsciences.org\/staging\/4414\/wp-json\/wp\/v2\/comments?post=6333"}],"version-history":[{"count":1,"href":"https:\/\/modernsciences.org\/staging\/4414\/wp-json\/wp\/v2\/posts\/6333\/revisions"}],"predecessor-version":[{"id":6334,"href":"https:\/\/modernsciences.org\/staging\/4414\/wp-json\/wp\/v2\/posts\/6333\/revisions\/6334"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/modernsciences.org\/staging\/4414\/wp-json\/wp\/v2\/media\/6325"}],"wp:attachment":[{"href":"https:\/\/modernsciences.org\/staging\/4414\/wp-json\/wp\/v2\/media?parent=6333"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/modernsciences.org\/staging\/4414\/wp-json\/wp\/v2\/categories?post=6333"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/modernsciences.org\/staging\/4414\/wp-json\/wp\/v2\/tags?post=6333"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}