可预测性
气候学
厄尔尼诺南方涛动
环境科学
航程(航空)
气候变化
热带大西洋
太平洋十年振荡
海面温度
海洋学
地质学
物理
材料科学
量子力学
复合材料
作者
Scott B. Power,Matthieu Lengaigne,Antonietta Capotondi,Myriam Khodri,Jérôme Vialard,Beyrem Jebri,Éric Guilyardi,Shayne McGregor,Jong‐Seong Kug,Matthew Newman,Michael J. McPhaden,Gerald A. Meehl,Doug Smith,Julia E. Cole,Julien Emile‐Geay,Daniel J. Vimont,Andrew T. Wittenberg,Matthew Collins,Geon-Il Kim,Wenju Cai
出处
期刊:Science
[American Association for the Advancement of Science]
日期:2021-09-30
卷期号:374 (6563)
被引量:153
标识
DOI:10.1126/science.aay9165
摘要
Climate variability in the tropical Pacific affects global climate on a wide range of time scales. On interannual time scales, the tropical Pacific is home to the El Niño–Southern Oscillation (ENSO). Decadal variations and changes in the tropical Pacific, referred to here collectively as tropical Pacific decadal variability (TPDV), also profoundly affect the climate system. Here, we use TPDV to refer to any form of decadal climate variability or change that occurs in the atmosphere, the ocean, and over land within the tropical Pacific. “Decadal,” which we use in a broad sense to encompass multiyear through multidecadal time scales, includes variability about the mean state on decadal time scales, externally forced mean-state changes that unfold on decadal time scales, and decadal variations in the behavior of higher-frequency modes like ENSO.
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