{"id":18549,"date":"2024-07-03T14:41:38","date_gmt":"2024-07-03T05:41:38","guid":{"rendered":"https:\/\/sdgs.kyushu-u.ac.jp\/?p=18549"},"modified":"2024-07-16T14:41:58","modified_gmt":"2024-07-16T05:41:58","slug":"early-onset-el-nino-means-warmer-winters-in-east-asia-and-vice-versa","status":"publish","type":"post","link":"https:\/\/sdgs.kyushu-u.ac.jp\/en\/18549","title":{"rendered":"Early-onset El Ni\u00f1o means warmer winters in East Asia, and vice versa"},"content":{"rendered":"

Post-doctoral Fellow Masahiro Shiozaki
\nDivision of Earth Environment Dynamics<\/span><\/strong><\/p>\n

Analyzing 100 different climate simulations over the past 61 years to find how El Ni\u00f1o determines warm or cold winters in Japan<\/h5>\n

Fukuoka, Japan\u2014The phenomenon known as El Ni\u00f1o can cause abnormal and extreme climate around the world due to it dramatically altering the normal flow of the atmosphere. In Japan, historical data has shown that El Ni\u00f1o years tend to lead to warmer winters. This case was exemplified recently with Japan\u2019s warm 2023-2024 winter season. However, there have also been cases of cold winters in Japan during El Ni\u00f1o years, such as the one recorded in 2014-2015. Yet, it was unclear as to why this was occurring.<\/p>\n

Publishing in the Journal of Climate, researchers from Kyushu University\u2019s Research Institute for Applied Mechanics have found that the early onset of El Ni\u00f1o around June leads to warm winter climates in East Asia, while the late onset of El Ni\u00f1o is associated with colder winters. The team hopes that their results can help better model winter climate patterns in East Asia during El Ni\u00f1o years, and lead to more accurate long-term climate predictions.<\/p>\n

El Ni\u00f1o is a climate pattern characterized by the warming of the tropical eastern Pacific Ocean caused by the weakening of equatorial trade winds that blow from the western coast of South America to the Philippines and Indonesia. In regular years, these trade winds would push the ocean\u2019s warmer waters westward leading to cooler waters rising in the east. These warmer western waters drive atmospheric convection generating clouds and rain.<\/p>\n

\u201cEach El Ni\u00f1o is individually unique, and no two El Ni\u00f1os are exactly alike,\u201d explains Post-doctoral Fellow Masahiro Shiozaki who authored the study. \u201cNaturally, these differences lead to a variety of abnormal global climate patterns. To better predict regional weather and climate during El Ni\u00f1o, it is important to know how and where the atmosphere changes.\u201d<\/p>\n

Shiozaki highlighted a case in Japan during the winter of 2023-2024. This was an El Ni\u00f1o year, and in Japan that tends to mean a warmer winter. And in fact, the winter of 2023-2024 was inordinately warm. However, this was not always the case. In the El Ni\u00f1o year of 2014-2015, Japan\u2019s winter was colder than average.<\/p>\n

\u201cJapanese winters are also influenced by the Arctic as well as strong natural variability inherent to the atmosphere. Because of these various effects, it has been challenging to identify how El Ni\u00f1o determines warm or cold winters in East Asia,\u201d continues Shiozaki. \u201cTo address this issue, we simulated the weather patterns of the past 61 years in 100 different ways by adding perturbations to the weather patterns. In this simulation, 1700 El Ni\u00f1o events occurred, and we calculated how the atmosphere changed each time. This method allowed us to reduce any atmospheric noise in the data, giving us a clearer view of El Ni\u00f1o\u2019s direct impact.\u201d<\/p>\n

The team\u2019s analysis found that it was not only El Ni\u00f1o, but also an anomalous warming of the tropical Indian Ocean that led to warmer East Asian winters. The early onset of El Ni\u00f1o around June effectively warmed the Indian Ocean from summer to winter. This ocean warming suppressed atmospheric convection over the tropical western Pacific, resulting in less rainfall and atmospheric heating.<\/p>\n

\u201cThe resulting reduction in atmospheric heating excited atmospheric waves that propagated into the western North Pacific, forming an anomalous anticyclonic circulation southeast of Japan,\u201d Shiozaki explains. \u201cAnomalous south-easterly winds from this circulation pattern weakened the northwesterly winter monsoon from the continent, leading to the warm winter climate in East Asia. On the other hand, cold Japanese winters are associated with a late onset of El Ni\u00f1o and no significant warming of the Indian Ocean.\u201d<\/p>\n

The team hopes their new findings will be utilized by researchers and meteorologists to better predict climate patterns months in advance, especially during active El Ni\u00f1o phases.<\/p>\n

\u201cThe influence of global warming is clear in the recent trend of warmer winters worldwide. The effects of rising water temperatures are especially evident in the Indian Ocean,\u201d concludes Professor Hiroki Tokinaga who led the research team. \u201cFurther research is needed to determine how global warming and other tropical climate phenomena will change future winters in East Asia.\u201d<\/p>\n

Research-related inquiries<\/h4>\n

Hiroki Tokinaga, Professor<\/a>Research Institute for Applied Mechanics Department
\nMasahiro Shiozaki, Post-doctoral Fellow<\/a>Research Institute for Applied Mechanics Department<\/p>\n

Contact information can also be found in the full release<\/a><\/p>\n","protected":false},"excerpt":{"rendered":"Post-doctoral Fellow Masahiro Shiozaki Division of Earth Environment Dynamics Analyzing 100 different climate simulations over the past 61 years to find how El Ni\u00f1o determines warm or cold winters in Japan Fukuoka, Japan\u2014The phenomenon known as El Ni\u00f1o can cause abnormal and extreme climate around the world due to it dramatically altering the normal flow […]","protected":false},"author":7,"featured_media":0,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":[],"categories":[33],"tags":[43],"acf":[],"aioseo_notices":[],"_links":{"self":[{"href":"https:\/\/sdgs.kyushu-u.ac.jp\/en\/wp-json\/wp\/v2\/posts\/18549"}],"collection":[{"href":"https:\/\/sdgs.kyushu-u.ac.jp\/en\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/sdgs.kyushu-u.ac.jp\/en\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/sdgs.kyushu-u.ac.jp\/en\/wp-json\/wp\/v2\/users\/7"}],"replies":[{"embeddable":true,"href":"https:\/\/sdgs.kyushu-u.ac.jp\/en\/wp-json\/wp\/v2\/comments?post=18549"}],"version-history":[{"count":5,"href":"https:\/\/sdgs.kyushu-u.ac.jp\/en\/wp-json\/wp\/v2\/posts\/18549\/revisions"}],"predecessor-version":[{"id":18555,"href":"https:\/\/sdgs.kyushu-u.ac.jp\/en\/wp-json\/wp\/v2\/posts\/18549\/revisions\/18555"}],"wp:attachment":[{"href":"https:\/\/sdgs.kyushu-u.ac.jp\/en\/wp-json\/wp\/v2\/media?parent=18549"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/sdgs.kyushu-u.ac.jp\/en\/wp-json\/wp\/v2\/categories?post=18549"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/sdgs.kyushu-u.ac.jp\/en\/wp-json\/wp\/v2\/tags?post=18549"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}