Pantropical climate interactions

IF 45.8 1区综合性期刊 Q1 MULTIDISCIPLINARY SCIENCES

Science Pub Date : 2019-03-01 DOI:10.1126/science.aav4236

Wenju Cai, Lixin Wu, Matthieu Lengaigne, Tim Li, Shayne McGregor, Jong-Seong Kug, Jin-Yi Yu, Malte F. Stuecker, Agus Santoso, Xichen Li, Yoo-Geun Ham, Yoshimitsu Chikamoto, Benjamin Ng, Michael J. McPhaden, Yan Du, Dietmar Dommenget, Fan Jia, Jules B. Kajtar, Noel Keenlyside, Xiaopei Lin, Jing-Jia Luo, Marta Martín-Rey, Yohan Ruprich-Robert, Guojian Wang, Shang-Ping Xie, Yun Yang, Sarah M. Kang, Jun-Young Choi, Bolan Gan, Geon-Il Kim, Chang-Eun Kim, Sunyoung Kim, Jeong-Hwan Kim, Ping Chang

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引用次数: 364

Abstract

The El Niño–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.

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泛热带气候的相互作用

厄尔尼诺-南方涛动（ENSO）起源于太平洋，是热带气候变化中最强烈和最著名的模式。它的影响范围遍及全球，可以通过扰动全球大气环流，迫使热带大西洋和印度洋的气候发生变化。热带大西洋和印度洋如何影响太平洋则较少被人关注。尤其值得注意的是 20 世纪 90 年代末开始的大西洋多年代变暖，因为最近的研究表明它影响了印度洋-太平洋气候、厄尔尼诺/南方涛动周期的特征以及全球地表变暖的间断。这些泛热带相互作用的发现为改进对当前气候中气候变异性的预测和完善不同人为作用力情景下的未来气候预测提供了一条途径。

本文章由计算机程序翻译，如有差异，请以英文原文为准。

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来源期刊

Science 综合性期刊-综合性期刊

CiteScore

61.10

自引率

0.90%

发文量

审稿时长

2.1 months

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