  {"id":170250,"date":"2022-12-12T09:01:13","date_gmt":"2022-12-12T19:01:13","guid":{"rendered":"https:\/\/www.hawaii.edu\/news\/?p=170250"},"modified":"2022-12-12T09:01:13","modified_gmt":"2022-12-12T19:01:13","slug":"el-nino-flavors","status":"publish","type":"post","link":"https:\/\/www.hawaii.edu\/news\/2022\/12\/12\/el-nino-flavors\/","title":{"rendered":"El Ni\u00f1o &lsquo;flavors&rsquo; help unravel past variability, future response to climate change"},"content":{"rendered":"<span class=\"span-reading-time rt-reading-time\" style=\"display: block;\"><span class=\"rt-label rt-prefix\">Reading time: <\/span> <span class=\"rt-time\"> 3<\/span> <span class=\"rt-label rt-postfix\">minutes<\/span><\/span><figure id=\"attachment_170260\" aria-describedby=\"caption-attachment-170260\" style=\"width: 676px\" class=\"wp-caption alignright\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/www.hawaii.edu\/news\/wp-content\/uploads\/2022\/12\/manoa-soest-el-nino-flavors.jpg\" alt=\"stream\" width=\"676\" height=\"381\" class=\"size-full wp-image-170260\" srcset=\"https:\/\/www.hawaii.edu\/news\/wp-content\/uploads\/2022\/12\/manoa-soest-el-nino-flavors.jpg 676w, https:\/\/www.hawaii.edu\/news\/wp-content\/uploads\/2022\/12\/manoa-soest-el-nino-flavors-300x169.jpg 300w, https:\/\/www.hawaii.edu\/news\/wp-content\/uploads\/2022\/12\/manoa-soest-el-nino-flavors-130x73.jpg 130w\" sizes=\"auto, (max-width: 676px) 100vw, 676px\" \/><figcaption id=\"caption-attachment-170260\" class=\"wp-caption-text\">Stream in Hilo. (Photo credit: Pascal Debrunner via Unsplash)<\/figcaption><\/figure>\n<p>As with many natural phenomena, scientists look to the climate of the past to understand what may lie ahead as Earth warms. By assessing so-called &lsquo;flavors&rsquo; of El Ni&#241;o events in historical records and model simulations, researchers have a clearer picture of El Ni&#241;o patterns over the past 12,000 years and are able to more accurately project future changes and impacts of this powerful force. The study, by scientists at the University of <span aria-label=\"Hawaii\">Hawai&#699;i<\/span> at M&#257;noa and University of Colorado Boulder, was published in <a href=\"https:\/\/www.nature.com\/articles\/s41467-022-34880-8\"><em>Nature Communications<\/em><\/a>.<\/p>\n<p>The new set of climate model simulations developed and analyzed by <strong>Christina Karamperidou<\/strong>, lead author of the study and associate professor at <abbr title=\"University of Hawaii\">ÌÇÐÄVlog¹Ù·½<\/abbr> M&#257;noa, and co-author Pedro DiNezio, associate professor at the University of Colorado Boulder, are the first to allow the study of changes in the frequency of El Ni&#241;o flavors during the past 12,000 years.<\/p>\n<figure id=\"attachment_170261\" aria-describedby=\"caption-attachment-170261\" style=\"width: 229px\" class=\"wp-caption alignright\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/www.hawaii.edu\/news\/wp-content\/uploads\/2022\/12\/manoa-soest-el-nino-flavors-2-1-229x300.png\" alt=\"el nino charts\" width=\"229\" height=\"300\" class=\"size-medium wp-image-170261\" srcset=\"https:\/\/www.hawaii.edu\/news\/wp-content\/uploads\/2022\/12\/manoa-soest-el-nino-flavors-2-1-229x300.png 229w, https:\/\/www.hawaii.edu\/news\/wp-content\/uploads\/2022\/12\/manoa-soest-el-nino-flavors-2-1-99x130.png 99w, https:\/\/www.hawaii.edu\/news\/wp-content\/uploads\/2022\/12\/manoa-soest-el-nino-flavors-2-1.png 300w\" sizes=\"auto, (max-width: 229px) 100vw, 229px\" \/><figcaption id=\"caption-attachment-170261\" class=\"wp-caption-text\">El Ni&#241;o flavors; Warm sea surface location: Eastern, Central or coastal. (Credit: Karamperidou, DiNezio 2022)<\/figcaption><\/figure>\n<p>This work offers new knowledge on how El Ni&#241;o may respond to climate change and thus can help reduce these uncertainties in global climate models and offer more accurate predictions of El Ni&#241;o impacts.<\/p>\n<p>&ldquo;We used a unique set of climate model simulations that span the Holocene, the past 12,000  years, and accounted for changes in the frequency of El Ni&#241;o flavors, the three preferred locations in which the peak of warming during different El Ni&#241;o events occur&#8212;eastern Pacific, central Pacific and coastal,&rdquo; said Karamperidou, associate professor of <a href=\"http:\/\/www.soest.hawaii.edu\/atmo\/\">atmospheric sciences<\/a> at the <abbr>ÌÇÐÄVlog¹Ù·½<\/abbr> M&#257;noa <a href=\"https:\/\/www.soest.hawaii.edu\/soestwp\/\">School of Ocean and Earth Science and Technology<\/a>. &ldquo;Doing this allowed us to reconcile conflicting records of past El Ni&#241;o behavior.&rdquo;<\/p>\n<p>El Ni&#241;o is the primary factor affecting variability in water temperature and trade wind strength in the Pacific. Typically, researchers look for indicators of El Ni&#241;o events in ancient, preserved material such as coral skeletons, Peruvian mollusk shells or lake sediment from the tropical Andes because locked within are indicators of past temperature and rainfall across Paci\ufb01c.<\/p>\n<p>&ldquo;However, depending on where the samples are taken from\u2014eastern Pacific, central Pacific, or near the South American coast\u2014the frequency of El Ni\u00f1o events appears to exhibit different patterns,&rdquo; said Karamperidou. &ldquo;Records from the eastern Pacific show an intensification of El Ni&#241;o activity from early to late Holocene, while records from the central Pacific show highly variable El Ni&#241;o throughout the Holocene.&rdquo;<\/p>\n<p>This enabled the researchers to test a <a href=\"https:\/\/agupubs.onlinelibrary.wiley.com\/doi\/10.1002\/2014PA002742\">hypothesis<\/a> that Karamperidou and colleagues posed in 2015&#8212;that paleoclimate records across the Pacific could be explained by changes in El Ni&#241;o flavors.<\/p>\n<p>&ldquo;Indeed, we showed that Eastern Pacific events have increased in frequency from early to late Holocene, while Central Pacific and coastal events have decreased in frequency, resulting in changes in the hydroclimate in the tropical Pacific,&rdquo; said Karamperidou. &ldquo;Importantly, we showed that it is not only their frequency, but also the strength of their impact that changes, which is important for interpreting records of past climate.&rdquo;<\/p>\n<h2>Connections to <span aria-label=\"Hawaii\u2019s\">Hawai&#699;i\u2019s<\/span> rainfall, hazards<\/h2>\n<p>El Ni&#241;o events have significant impacts on <span aria-label=\"Hawaii\u2019s\">Hawai&#699;i\u2019s<\/span> rainfall, trade wind strength, the probability of hurricane formation and drought, and the type of El Ni&#241;o event matters for these impacts.<\/p>\n<p>&ldquo;This information is important for water resource managers among others to better prepare for <span aria-label=\"Hawaii\">Hawai&#699;i<\/span> regional climate,&rdquo; said Karamperidou. &ldquo;So, it is imperative that we gain a better understanding of the mechanisms of these flavors, and also improve their representation in climate models and assess their projected changes under future climate conditions.&rdquo;<\/p>\n<h2>Surprising impacts<\/h2>\n<p>Additionally, this is the first study into the response of coastal El Ni&#241;o events to climate changes. During these events the sea surface warming is confined off the coast of South America while the conditions in the rest of the Pacific basin are normal or colder than normal.<\/p>\n<p>&ldquo;These coastal events have supersized impacts with severe flooding and disasters in countries like Peru and Ecuador,&rdquo; said Karamperidou. &ldquo;In fact, we showed in another recent <a href=\"https:\/\/agupubs.onlinelibrary.wiley.com\/doi\/10.1029\/2022GL098859\">paper<\/a> that even though these events are not felt around the globe like the more widely known Eastern and Central Pacific events, a better understanding of the mechanisms that drive them is essential for understanding the drivers of the other two flavors, as well.&rdquo;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>This work offers new knowledge on how El Ni&#241;o may respond to climate change.<\/p>\n","protected":false},"author":16,"featured_media":0,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[30],"tags":[745,93,1363,1314,158,92,73,9],"class_list":["post-170250","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-research","tag-atmospheric-sciences","tag-climate-change","tag-manoa-research","tag-manoa-sustainability","tag-publication","tag-school-of-ocean-and-earth-science-and-technology","tag-sustainability","tag-uh-manoa","entry","has-media"],"aioseo_notices":[],"jetpack_featured_media_url":"","_links":{"self":[{"href":"https:\/\/www.hawaii.edu\/news\/wp-json\/wp\/v2\/posts\/170250","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.hawaii.edu\/news\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.hawaii.edu\/news\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.hawaii.edu\/news\/wp-json\/wp\/v2\/users\/16"}],"replies":[{"embeddable":true,"href":"https:\/\/www.hawaii.edu\/news\/wp-json\/wp\/v2\/comments?post=170250"}],"version-history":[{"count":11,"href":"https:\/\/www.hawaii.edu\/news\/wp-json\/wp\/v2\/posts\/170250\/revisions"}],"predecessor-version":[{"id":170265,"href":"https:\/\/www.hawaii.edu\/news\/wp-json\/wp\/v2\/posts\/170250\/revisions\/170265"}],"wp:attachment":[{"href":"https:\/\/www.hawaii.edu\/news\/wp-json\/wp\/v2\/media?parent=170250"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.hawaii.edu\/news\/wp-json\/wp\/v2\/categories?post=170250"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.hawaii.edu\/news\/wp-json\/wp\/v2\/tags?post=170250"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}