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Pantropical climate interactions

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Title
Pantropical climate interactions
Author(s)
Cai, WJ; Wu, LX; Lengaigne, M; Li, T; McGregor, S; Kug, JS; Yu, JY; Malte F. Stuecker; Santoso, A; Li, XC; Ham, YG; Chikamoto, Y; Ng, B; McPhaden, MJ; Du, Y; Dommenget, D; Jia, F; Kajtar, JB; Keenlyside, N; Lin, XP; Luo, JJ; Martin-Rey, M; Ruprich-Robert, Y; Wang, GJ; Xie, SP; Yang, Y; Kang, SM; Choi, JY; Gan, BL; Kim, GI; Kim, CE; Kim, S; Kim, JH; Chang, P
Publication Date
2019-03
Journal
SCIENCE, v.363, no.6430, pp.944 - +
Publisher
AMER ASSOC ADVANCEMENT SCIENCE
Abstract
The El Nino-Southern Oscillation (ENSO), which originates in the Pacific, is the strongest and most well-known mode of tropical climate variability. Its reach is global, and it can force climate variations of the tropical Atlantic and Indian Oceans by perturbing the global atmospheric circulation. Less appreciated is how the tropical Atlantic and Indian Oceans affect the Pacific. Especially noteworthy is the multidecadal Atlantic warming that began in the late 1990s, because recent research suggests that it has influenced Indo-Pacific climate, the character of the ENSO cycle, and the hiatus in global surface warming. Discovery of these pantropical interactions provides a pathway forward for improving predictions of climate variability in the current climate and for refining projections of future climate under different anthropogenic forcing scenarios. © The Authors
URI
https://pr.ibs.re.kr/handle/8788114/6316
ISSN
0036-8075
Appears in Collections:
Center for Climate Physics(기후물리 연구단) > Journal Papers (저널 논문)
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