Marta Martín-Rey, Benjamin Ng, Yun Yang, Bolan Gan, Xiaopei Lin, Malte F. Stuecker, Guojian Wang, Jing-Jia Luo, Yan Du, Dietmar Dommenget, Noel Keenlyside, Wenju Cai, Fan Jia, Yoo-Geun Ham, Sarah M. Kang, Jeong-Hwan Kim, Agus Santoso, Ping Chang, Jun-Young Choi, Jules B. Kajtar, Tim Li, Jin-Yi Yu, Sun-Young Kim, Matthieu Lengaigne, Xichen Li, Geon-Il Kim, Shayne McGregor, Jong-Seong Kug, Michael J. McPhaden, Yoshimitsu Chikamoto, Lixin Wu, Chang Eun Kim, Shang-Ping Xie, Yohan Ruprich-Robert, Barcelona Supercomputing Center, Commonwealth Scientific and Industrial Research Organisation [Canberra] (CSIRO), Qingdao National Laboratory for Marine Science and Technology, Océan et variabilité du climat (VARCLIM), Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (LOCEAN), Institut Pierre-Simon-Laplace (IPSL (FR_636)), École normale supérieure - Paris (ENS Paris), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X)-Centre National d'Études Spatiales [Toulouse] (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université de Paris (UP)-École normale supérieure - Paris (ENS Paris), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X)-Centre National d'Études Spatiales [Toulouse] (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université de Paris (UP)-Institut de Recherche pour le Développement (IRD)-Muséum national d'Histoire naturelle (MNHN)-Centre National de la Recherche Scientifique (CNRS)-Sorbonne Université (SU)-Institut Pierre-Simon-Laplace (IPSL (FR_636)), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X)-Centre National d'Études Spatiales [Toulouse] (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université de Paris (UP)-Institut de Recherche pour le Développement (IRD)-Muséum national d'Histoire naturelle (MNHN)-Centre National de la Recherche Scientifique (CNRS)-Sorbonne Université (SU), School of Ocean and Earth Science and Technology (SOEST), University of Hawai‘i [Mānoa] (UHM), Pohang University of Science and Technology (POSTECH), Department of Atmospheric Sciences [Seattle], University of Washington [Seattle], Climate Change Research Centre, ARC Centre of Excellence for Climate System Science, University of New South Wales, Level 4 Matthews Bldg., Kensington, NSW 2052, Australia, Department of Plants, Soils and Climate, Utah State University (USU), NOAA Pacific Marine Environmental Laboratory [Seattle] (PMEL), National Oceanic and Atmospheric Administration (NOAA), South China Sea Institute of Oceanology, School of Earth, Atmosphere and Environment, Monash University, Monash University [Clayton], University of Chinese Academy of Sciences [Beijing] (UCAS), Key Laboratory of Ocean Circulation and Waves, CAS Institute of Oceanology (IOCAS), Chinese Academy of Sciences [Beijing] (CAS)-Chinese Academy of Sciences [Beijing] (CAS), College of Engineering, Mathematics and Physical Sciences [Exeter] (EMPS), University of Exeter, Nansen-Tutu Center for Marine Environmental Research, University of Cape Town, Key Laboratory of Meteorological Disaster [Nanjing University] (KLME - NUIST), Nanjing University of Information Science and Technology (NUIST), CSIC Instituto de Ciencias del Mar, Barcelona Supercomputing Center - Centro Nacional de Supercomputacion (BSC - CNS), Climate, Atmospheric Science and Physical Oceanography Department [La Jolla] (CASPO), Scripps Institution of Oceanography (SIO), University of California [San Diego] (UC San Diego), University of California-University of California-University of California [San Diego] (UC San Diego), University of California-University of California, Ulsan National Institute of Science and Technology (UNIST), University of Regina, Okinawa Institute of Science and Technology Graduate University (OIST), ANR-15-JCLI-0004,GOTHAM,Globally Observed Teleconnections and their role and representation in Hierarchies of Atmospheric Models(2015), Ministerio de Ciencia, Innovación y Universidades (España), Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636)), École normale supérieure - Paris (ENS-PSL), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X)-Centre National d'Études Spatiales [Toulouse] (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité)-École normale supérieure - Paris (ENS-PSL), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-École polytechnique (X)-Centre National d'Études Spatiales [Toulouse] (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité)-Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636)), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-École polytechnique (X)-Centre National d'Études Spatiales [Toulouse] (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité), School of Earth, Atmosphere and Environment, Scripps Institution of Oceanography (SIO - UC San Diego), University of California (UC)-University of California (UC)-University of California [San Diego] (UC San Diego), and University of California (UC)-University of California (UC)
12 pages, 5 figures, 1 box, 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, W.C. is supported by National Key R&D Program of China (2018YFA0605700). L.W., Xia.L., and B.G. are supported by the National Natural Science Foundation of China (NSFC) projects (41490643, 41490640, U1606402, and 41521091). W.C., G.W., B.N., and A.S. are supported by CSHOR and the Earth System and Climate Change Hub of the Australian Government’s National Environment Science Program. CSHOR is a joint research Centre for Southern Hemisphere Oceans Research between QNLM and CSIRO. M.L. is supported by the GOTHAM Belmont project (ANR-15-JCLI-0004-01) and the ARiSE ANR project. T.L. is supported by NSFC 41630423 and NSF AGS-1565653 grants. S.M. is supported by the Australian Research Council (ARC) through grant number FT160100162. J.-S.K. was supported by a National Research Foundation of Korea (NRF) grant funded by the Korea government (MSIT) (NRF-2018R1A5A1024958). J.-Y.Y. is supported by NSF AGS-1505145 and AGS-1833075 grants. M.F.S is supported by the Institute for Basic Science (project code IBS-R028-D1). Y.-G.H. is funded by the Korea Meteorological Administration Research and Development Program under grant KMI2018-03214. M.J.M is supported by NOAA and PMEL contribution number 4838. Y.D. is supported by the National Natural Science Foundation of China (41525019, 41830538, and 41521005) and the State Oceanic Administration of China (GASI-IPOVAI-02). D.D. is supported by ARC grant number CE170100023. M.M.-R. has been supported by the MORDICUS grant under contract ANR-13-762 SENV-0002-01 and CGL2017-86415-R. Y.R.-R. is supported by an 800154-INADEC individual MSCA-IF-EF-ST grant. S.-P.X. is supported by the NSF. J.B.K. was supported by the National Environment Research Council (NE/N005783/1)