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El Nino-Southern Oscillation complexity

Author(s)
Timmermann, AxelAn, Soon-IlKug, Jong-SeongJin, Fei-FeiCai, WenjuCapotondi, AntoniettaCobb, KimLengaigne, MatthieuMcPhaden, Michael J.Stuecker, Malte F.Stein, KarlWittenberg, Andrew T.Yun, Kyung-SookBayr, TobiasChen, Han-ChingChikamoto, YoshimitsuDewitte, BorisDommenget, DietmarGrothe, PamelaGuilyardi, EricHam, Yoo-GeunHayashi, MichiyaIneson, SarahKang, DaehyunKim, SunyongKim, WonMooLee, June-YiLi, TimLuo, Jing-JiaMcGregor, ShaynePlanton, YannPower, ScottRashid, HarunRen, Hong-LiSantoso, AgusTakahashi, KenTodd, AlexanderWang, GuominWang, GuojianXie, RuihuangYang, Woo-HyunYeh, Sang-WookYoon, JinhoZeller, ElkeZhang, Xuebin
Issued Date
2018-07
DOI
10.1038/s41586-018-0252-6
URI
https://scholarworks.unist.ac.kr/handle/201301/24719
Fulltext
https://www.nature.com/articles/s41586-018-0252-6
Citation
NATURE, v.559, no.7715, pp.535 - 545
Abstract
El Nino events are characterized by surface warming of the tropical Pacific Ocean and weakening of equatorial trade winds that occur every few years. Such conditions are accompanied by changes in atmospheric and oceanic circulation, affecting global climate, marine and terrestrial ecosystems, fisheries and human activities. The alternation of warm El Nino and cold La Nina conditions, referred to as the El Nino-Southern Oscillation (ENSO), represents the strongest year-to-year fluctuation of the global climate system. Here we provide a synopsis of our current understanding of the spatio-temporal complexity of this important climate mode and its influence on the Earth system
Publisher
NATURE PUBLISHING GROUP
ISSN
0028-0836
Keyword
SEA-SURFACE TEMPERATUREGENERAL-CIRCULATION MODELPACIFIC CONVERGENCE ZONEWESTERLY WIND EVENTSNINO/SOUTHERN OSCILLATIONEQUATORIAL PACIFICCOMBINATION-MODEMERIDIONAL MODELA-NINAENSO

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