| Literature DB >> 34591645 |
Scott Power1,2,3, Matthieu Lengaigne4, Antonietta Capotondi5,6, Myriam Khodri7, Jérôme Vialard7, Beyrem Jebri7, Eric Guilyardi7,8, Shayne McGregor2, Jong-Seong Kug9, Matthew Newman5,6, Michael J McPhaden10, Gerald Meehl11, Doug Smith12, Julia Cole13, Julien Emile-Geay14, Daniel Vimont15, Andrew T Wittenberg16, Mat Collins17, Geon-Il Kim9, Wenju Cai18,19,20, Yuko Okumura21, Christine Chung22, Kim M Cobb23, François Delage22, Yann Y Planton10, Aaron Levine10, Feng Zhu21, Janet Sprintall24, Emanuele Di Lorenzo25, Xuebin Zhang18, Jing-Jia Luo26, Xiaopei Lin19,20, Magdalena Balmaseda27, Guojian Wang18, Benjamin J Henley2,3,28.
Abstract
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.Entities:
Year: 2021 PMID： 34591645 DOI： 10.1126/science.aay9165
Source DB: PubMed Journal: Science ISSN： 0036-8075 Impact factor: 47.728