{"id":23640,"date":"2022-11-26T22:24:25","date_gmt":"2022-11-26T16:39:25","guid":{"rendered":"https:\/\/www.revoscience.com\/en\/?p=23640"},"modified":"2022-11-26T22:25:10","modified_gmt":"2022-11-26T16:40:10","slug":"earths-orbit-is-more-important-in-driving-tropical-pacific-climate-than-previously-thought","status":"publish","type":"post","link":"https:\/\/www.revoscience.com\/en\/earths-orbit-is-more-important-in-driving-tropical-pacific-climate-than-previously-thought\/","title":{"rendered":"Earth\u2019s orbit is more important in driving tropical Pacific climate than previously thought"},"content":{"rendered":"\n<p>MADISON\u2014For years, the prevailing belief among climate scientists was that Earth\u2019s tilt was the primary factor in determining seasonal climate in the tropical Pacific. <\/p>\n\n\n\n<p>But new research from scientists at the University of Wisconsin\u2013Madison and several other institutions around the world highlights an overlooked factor that has an equally important role: the \u201cdistance effect\u201d of Earth\u2019s orbit, which affects the planet\u2019s proximity to the sun.<\/p>\n\n\n\n<p>\u201cYou\u2019d think that our understanding of the seasons is pretty well established. But right on the equator in the tropical Pacific, we have a lot of trouble simulating the seasonal cycle,\u201d says Daniel Vimont, a climate scientist at UW\u2013Madison and collaborating author of the paper.<\/p>\n\n\n\n<figure class=\"wp-block-image size-full is-resized\"><img loading=\"lazy\" decoding=\"async\" sizes=\"auto, (max-width: 620px) 100vw, 620px\" src=\"https:\/\/www.revoscience.com\/en\/wp-content\/uploads\/2022\/11\/atmosphereoceancoupling.jpeg\" alt=\"\" class=\"wp-image-23641\" width=\"839\" height=\"559\" title=\"\" srcset=\"https:\/\/www.revoscience.com\/en\/wp-content\/uploads\/2022\/11\/atmosphereoceancoupling.jpeg 620w, https:\/\/www.revoscience.com\/en\/wp-content\/uploads\/2022\/11\/atmosphereoceancoupling-600x400.jpeg 600w, https:\/\/www.revoscience.com\/en\/wp-content\/uploads\/2022\/11\/atmosphereoceancoupling-174x116.jpeg 174w\" \/><figcaption class=\"wp-element-caption\">The atmosphere and ocean interact through exchanges of heat and momentum. When warm water and clouds move from west to east in the tropical Pacific during a climate event like El Ni\u00f1o, it changes the weather that happens on a global scale.&nbsp;<strong>IMAGE: NOAA<\/strong><\/figcaption><\/figure>\n\n\n\n<p>He explains that closing this gap is important for understanding the tropical Pacific because it\u2019s a critical region that influences the rest of Earth\u2019s climate system.<\/p>\n\n\n\n<p>For instance, it\u2019s where El Ni\u00f1o occurs, a climate pattern Vimont describes as the biggest thing that can happen in Earth\u2019s climate system on year-to-year time scales. During El Ni\u00f1o events, winds push warm water from the Western Pacific toward the Eastern, bringing with it warmer surface conditions, and decreased upwelling of nutrient-rich, cold water that affects what marine species can flourish where.<\/p>\n\n\n\n<p>Since the ocean and atmosphere are also connected, when warm water and clouds move from west to east during a climate event like El Ni\u00f1o, it changes the weather that happens on a global scale, too.<\/p>\n\n\n\n<p>The equator is also the perfect place to isolate the impact of the Earth\u2019s orbit from its tilt since the effects of the Earth\u2019s tilt are minimized on the equator (the effects are strongest at the poles).<\/p>\n\n\n\n<p>Vimont and his lab were already modeling this ocean-atmosphere connection when they were asked to join the study led by John C. H. Chiang of the University of California, Berkeley, which was recently published in Nature. The researchers revealed that both the \u201ctilt effect\u201d and the \u201cdistance effect\u201d play equally important roles in influencing climate seasonality in the Pacific.<\/p>\n\n\n\n<p>It just so happens that in the tropical Pacific\u2019s current climate the two cycles are aligned, obscuring the full weight of influence the distance effect has and making it seem like the Earth\u2019s tilt had an outsized role in determining the seasons.<\/p>\n\n\n\n<p>For the study, Vimont used computer simulations to \u201cbreak the physics\u201d of the real world to model how the ocean and the atmosphere interact and influence the timing of the seasonal cycle in the tropical Pacific. He was also interested in determining what processes are vital to creating our climates.<\/p>\n\n\n\n<p>\u201cThe atmosphere and the ocean interact with each other by means of exchanging heat. But they also exchange momentum, so the atmosphere can push on the ocean,\u201d Vimont says. \u201cSo, one thing you might do is say, \u2018Well, I&#8217;m not going to let the atmosphere push on the ocean.\u2019\u201d<\/p>\n\n\n\n<p>By using models to toggle different processes on and off, climate scientists can get a sense for which processes influence climate. In this case, they found that the atmosphere and ocean pushing on each other is important in creating the climate on the tropical Pacific.<\/p>\n\n\n\n<p>\u201cThat&#8217;s important because as we look back in the past, this new finding suggests we should revisit model simulations and paleoclimatic data that we use to infer past behavior of the tropical Pacific,\u201d Vimont says.<\/p>\n\n\n\n<p>Since the Earth\u2019s orbit is elliptical and changes through time, that means in the past this second seasonal cycle driven by the Earth\u2019s distance from the sun could have been timed differently from the cycle driven by the Earth\u2019s tilt.<\/p>\n\n\n\n<p>These results provide a chance to test global climate model simulations of past changes to climate. While natural climate cycles caused by Earth\u2019s orbit and tilt have long existed and influenced the planet, the changes driven by human influences since the start of the industrial era cannot be explained by these natural cycles.<\/p>\n\n\n\n<p>Understanding how these human influences alter the Earth\u2019s climate in the future is another focus of climate scientists. They use models of past climates to project and plan for the future, so improving scientific understanding of these models of the past is particularly important.<\/p>\n\n\n\n<p>\u201cThis study is a great opportunity to push our understanding of the tropical Pacific, which we know affects the rest of the world,\u201d Vimont says.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>For years, the prevailing belief among climate scientists was that Earth\u2019s tilt was the primary factor in determining seasonal climate in the tropical Pacific. <\/p>\n","protected":false},"author":2,"featured_media":23641,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[3],"tags":[],"class_list":["post-23640","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-news"],"featured_image_urls":{"full":["https:\/\/www.revoscience.com\/en\/wp-content\/uploads\/2022\/11\/atmosphereoceancoupling.jpeg",620,413,false],"thumbnail":["https:\/\/www.revoscience.com\/en\/wp-content\/uploads\/2022\/11\/atmosphereoceancoupling-200x200.jpeg",200,200,true],"medium":["https:\/\/www.revoscience.com\/en\/wp-content\/uploads\/2022\/11\/atmosphereoceancoupling-600x400.jpeg",600,400,true],"medium_large":["https:\/\/www.revoscience.com\/en\/wp-content\/uploads\/2022\/11\/atmosphereoceancoupling.jpeg",620,413,false],"large":["https:\/\/www.revoscience.com\/en\/wp-content\/uploads\/2022\/11\/atmosphereoceancoupling.jpeg",620,413,false],"1536x1536":["https:\/\/www.revoscience.com\/en\/wp-content\/uploads\/2022\/11\/atmosphereoceancoupling.jpeg",620,413,false],"2048x2048":["https:\/\/www.revoscience.com\/en\/wp-content\/uploads\/2022\/11\/atmosphereoceancoupling.jpeg",620,413,false],"ultp_layout_landscape_large":["https:\/\/www.revoscience.com\/en\/wp-content\/uploads\/2022\/11\/atmosphereoceancoupling.jpeg",620,413,false],"ultp_layout_landscape":["https:\/\/www.revoscience.com\/en\/wp-content\/uploads\/2022\/11\/atmosphereoceancoupling.jpeg",620,413,false],"ultp_layout_portrait":["https:\/\/www.revoscience.com\/en\/wp-content\/uploads\/2022\/11\/atmosphereoceancoupling-600x413.jpeg",600,413,true],"ultp_layout_square":["https:\/\/www.revoscience.com\/en\/wp-content\/uploads\/2022\/11\/atmosphereoceancoupling-600x413.jpeg",600,413,true],"newspaper-x-single-post":["https:\/\/www.revoscience.com\/en\/wp-content\/uploads\/2022\/11\/atmosphereoceancoupling.jpeg",620,413,false],"newspaper-x-recent-post-big":["https:\/\/www.revoscience.com\/en\/wp-content\/uploads\/2022\/11\/atmosphereoceancoupling-550x360.jpeg",550,360,true],"newspaper-x-recent-post-list-image":["https:\/\/www.revoscience.com\/en\/wp-content\/uploads\/2022\/11\/atmosphereoceancoupling-95x65.jpeg",95,65,true],"web-stories-poster-portrait":["https:\/\/www.revoscience.com\/en\/wp-content\/uploads\/2022\/11\/atmosphereoceancoupling.jpeg",620,413,false],"web-stories-publisher-logo":["https:\/\/www.revoscience.com\/en\/wp-content\/uploads\/2022\/11\/atmosphereoceancoupling.jpeg",96,64,false],"web-stories-thumbnail":["https:\/\/www.revoscience.com\/en\/wp-content\/uploads\/2022\/11\/atmosphereoceancoupling.jpeg",150,100,false]},"author_info":{"info":["RevoScience"]},"category_info":"<a href=\"https:\/\/www.revoscience.com\/en\/category\/news\/\" rel=\"category tag\">News<\/a>","tag_info":"News","comment_count":"0","_links":{"self":[{"href":"https:\/\/www.revoscience.com\/en\/wp-json\/wp\/v2\/posts\/23640","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.revoscience.com\/en\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.revoscience.com\/en\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.revoscience.com\/en\/wp-json\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"https:\/\/www.revoscience.com\/en\/wp-json\/wp\/v2\/comments?post=23640"}],"version-history":[{"count":0,"href":"https:\/\/www.revoscience.com\/en\/wp-json\/wp\/v2\/posts\/23640\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/www.revoscience.com\/en\/wp-json\/wp\/v2\/media\/23641"}],"wp:attachment":[{"href":"https:\/\/www.revoscience.com\/en\/wp-json\/wp\/v2\/media?parent=23640"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.revoscience.com\/en\/wp-json\/wp\/v2\/categories?post=23640"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.revoscience.com\/en\/wp-json\/wp\/v2\/tags?post=23640"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}