  {"id":133580,"date":"2021-01-10T09:00:10","date_gmt":"2021-01-10T19:00:10","guid":{"rendered":"https:\/\/www.hawaii.edu\/news\/?p=133580"},"modified":"2021-01-11T10:31:27","modified_gmt":"2021-01-11T20:31:27","slug":"hawaii-drought-el-nino-winter","status":"publish","type":"post","link":"https:\/\/www.hawaii.edu\/news\/2021\/01\/10\/hawaii-drought-el-nino-winter\/","title":{"rendered":"Hawai\u02bbi drought during El Ni\u00f1o winter? Not always"},"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\"> 2<\/span> <span class=\"rt-label rt-postfix\">minutes<\/span><\/span><figure id=\"attachment_133603\" aria-describedby=\"caption-attachment-133603\" style=\"width: 676px\" class=\"wp-caption alignright\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/www.hawaii.edu\/news\/wp-content\/uploads\/2021\/01\/manoa-soest-el-nino-drought.jpg\" alt=\"stream\" width=\"676\" height=\"381\" class=\"size-full wp-image-133603\" srcset=\"https:\/\/www.hawaii.edu\/news\/wp-content\/uploads\/2021\/01\/manoa-soest-el-nino-drought.jpg 676w, https:\/\/www.hawaii.edu\/news\/wp-content\/uploads\/2021\/01\/manoa-soest-el-nino-drought-300x169.jpg 300w, https:\/\/www.hawaii.edu\/news\/wp-content\/uploads\/2021\/01\/manoa-soest-el-nino-drought-130x73.jpg 130w\" sizes=\"auto, (max-width: 676px) 100vw, 676px\" \/><figcaption id=\"caption-attachment-133603\" class=\"wp-caption-text\"><span aria-label=\"Hawaii's\">Hawai&#699;i&#8217;s<\/span> freshwater resources are intricately linked to rainfall patterns. (Photo credit: <abbr>DLNR<\/abbr>)<\/figcaption><\/figure>\n<p>El Ni&#241;o events have long been perceived as a driver for low rainfall in the winter and spring in <span aria-label=\"Hawaii,\">Hawai&#699;i,<\/span> creating a six-month wet-season drought. However, the connection between <span aria-label=\"Hawaii\">Hawai&#699;i<\/span> winter rainfall and El Ni&#241;o is not as straightforward as previously thought, according to a recent <a href=\"https:\/\/journals.ametsoc.org\/view\/journals\/clim\/33\/22\/jcliD190985.xml?tab_body=fulltext-display\">study<\/a> by researchers in the University of <span aria-label=\"Hawaii\">Hawai&#699;i<\/span> at M&#257;noa <a href=\"https:\/\/www.soest.hawaii.edu\/soestwp\/\">School of Ocean and Earth Science and Technology<\/a> (<abbr>SOEST<\/abbr>).<\/p>\n<p>Studies in the past decade suggested that there are at least two types of El Ni&#241;o: the Eastern Pacific and Central Pacific, when the warmest pool of water is located in the eastern or central portions of the ocean basin, respectively. El Ni&#241;o events usually begin in summer and last for about one year.<\/p>\n<p><a href=\"http:\/\/www.soest.hawaii.edu\/atmo\/\">Atmospheric scientists<\/a> at <abbr>ÌÇÐÄVlog¹Ù·½<\/abbr> M&#257;noa analyzed data on the large-scale circulation patterns over the eastern and central Pacific to find that <span aria-label=\"Hawaii\">Hawai&#699;i<\/span> drought is only associated with the Eastern Pacific El Ni&#241;o. For the Central Pacific El Ni&#241;o events, deficient rainfall in <span aria-label=\"Hawaii\">Hawai&#699;i<\/span> occurred only 60% of the time. Therefore, a winter drought is not guaranteed following a Central Pacific El Ni&#241;o.<\/p>\n<figure id=\"attachment_133602\" aria-describedby=\"caption-attachment-133602\" style=\"width: 300px\" class=\"wp-caption alignright\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/www.hawaii.edu\/news\/wp-content\/uploads\/2021\/01\/manoa-soest-el-nino-drought-2-300x169.jpg\" alt=\"people working outside\" width=\"300\" height=\"169\" class=\"size-medium wp-image-133602\" srcset=\"https:\/\/www.hawaii.edu\/news\/wp-content\/uploads\/2021\/01\/manoa-soest-el-nino-drought-2-300x169.jpg 300w, https:\/\/www.hawaii.edu\/news\/wp-content\/uploads\/2021\/01\/manoa-soest-el-nino-drought-2-130x73.jpg 130w, https:\/\/www.hawaii.edu\/news\/wp-content\/uploads\/2021\/01\/manoa-soest-el-nino-drought-2.jpg 676w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><figcaption id=\"caption-attachment-133602\" class=\"wp-caption-text\"><span aria-label=\"Hawaii\">Hawai&#699;i<\/span> agriculture is dependent on ample rainfall in the region. (Photo credit: Corey Rothwell)<\/figcaption><\/figure>\n<h2>Critical for planning and water resource management<\/h2>\n<p>The differences in how the Eastern and Central Pacific El Ni&#241;o affect rainfall can be critical for proper planning and water resource management.<\/p>\n<p>&ldquo;This new result is a boon for many agencies in <span aria-label=\"Hawaii,\">Hawai&#699;i,<\/span> for example, the Board of Water Supply, <span aria-label=\"Hawaii\">Hawai&#699;i<\/span> Department of Land and Natural Resources, and <span aria-label=\"Hawaii\">Hawai&#699;i<\/span> Department of Agriculture,&rdquo; said <strong>Pao-Shin Chu<\/strong>, a <abbr>SOEST<\/abbr> professor, <span aria-label=\"Hawaii\">Hawai&#699;i<\/span> state climatologist and co-author of the study. &ldquo;Beyond these agencies, ranchers, flower growers and other stakeholders that are concerned with the relationship between El Ni&#241;o and water supply in <span aria-label=\"Hawaii\">Hawai&#699;i<\/span> may also benefit from the new findings.&rdquo;<\/p>\n<p>Given that El Ni&#241;o is a recurring phenomenon, knowing the type of El Ni&#241;o that occurs will allow researchers and resource managers to more easily evaluate and prepare for Hawaiian regional climate in winter.<\/p>\n<p>For more information see <a href=\"https:\/\/www.soest.hawaii.edu\/soestwp\/announce\/news\/hawaii-drought-during-el-nino-winter-not-always-according-to-new-research\/\"><abbr>SOEST<\/abbr>\u2019s website<\/a>.<\/p>\n<p><em>&#8211;By Marcie Grabowski<\/em><\/p>\n","protected":false},"excerpt":{"rendered":"<p><abbr>ÌÇÐÄVlog¹Ù·½<\/abbr> research revealed the connection between <span aria-label=\"Hawaii\">Hawai&#699;i<\/span> winter rainfall and El Ni&#241;o is not as straightforward as previously thought.<\/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":[745,1363,158,92,9],"class_list":["post-133580","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-research","tag-atmospheric-sciences","tag-manoa-research","tag-publication","tag-school-of-ocean-and-earth-science-and-technology","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\/133580","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=133580"}],"version-history":[{"count":10,"href":"https:\/\/www.hawaii.edu\/news\/wp-json\/wp\/v2\/posts\/133580\/revisions"}],"predecessor-version":[{"id":133690,"href":"https:\/\/www.hawaii.edu\/news\/wp-json\/wp\/v2\/posts\/133580\/revisions\/133690"}],"wp:attachment":[{"href":"https:\/\/www.hawaii.edu\/news\/wp-json\/wp\/v2\/media?parent=133580"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.hawaii.edu\/news\/wp-json\/wp\/v2\/categories?post=133580"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.hawaii.edu\/news\/wp-json\/wp\/v2\/tags?post=133580"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}