El Niño–Southern Oscillation complexity

被引:0
|
作者
Axel Timmermann
Soon-Il An
Jong-Seong Kug
Fei-Fei Jin
Wenju Cai
Antonietta Capotondi
Kim M. Cobb
Matthieu Lengaigne
Michael J. McPhaden
Malte F. Stuecker
Karl Stein
Andrew T. Wittenberg
Kyung-Sook Yun
Tobias Bayr
Han-Ching Chen
Yoshimitsu Chikamoto
Boris Dewitte
Dietmar Dommenget
Pamela Grothe
Eric Guilyardi
Yoo-Geun Ham
Michiya Hayashi
Sarah Ineson
Daehyun Kang
Sunyong Kim
WonMoo Kim
June-Yi Lee
Tim Li
Jing-Jia Luo
Shayne McGregor
Yann Planton
Scott Power
Harun Rashid
Hong-Li Ren
Agus Santoso
Ken Takahashi
Alexander Todd
Guomin Wang
Guojian Wang
Ruihuang Xie
Woo-Hyun Yang
Sang-Wook Yeh
Jinho Yoon
Elke Zeller
Xuebin Zhang
机构
[1] Institute for Basic Science (IBS),Center for Climate Physics
[2] Pusan National University,International Pacific Research Center
[3] University of Hawaii at Manoa,Department of Atmospheric Sciences
[4] Yonsei University,Division of Environmental Science and Engineering
[5] Pohang University of Science and Technology (POSTECH),Department of Atmospheric Science, SOEST
[6] University of Hawaii at Manoa,Physical Oceanography Laboratory/CIMST
[7] CSIRO Oceans and Atmosphere,Centre for Southern Hemisphere Oceans Research (CSHOR)
[8] Ocean University of China and Qingdao National Laboratory for Marine Science and Technology,Cooperative Institute for Research in Environmental Science
[9] CSIRO Oceans and Atmosphere,Physical Sciences Division
[10] University of Colorado,Earth and Atmospheric Sciences
[11] NOAA Earth System Research Laboratory,LOCEAN/IPSL
[12] Georgia Tech,Department of Atmospheric Sciences
[13] Sorbonne Universités/UPMC-CNRS-IRD-MNHN,Cooperative Programs for the Advancement of Earth System Science
[14] Pacific Marine Environmental Laboratory/NOAA,Department of Atmospheric Sciences
[15] University of Washington,Department of Plants, Soils, and Climate
[16] University Corporation for Atmospheric Research,School of Earth, Atmosphere and Environment
[17] Geophysical Fluid Dynamics Laboratory/NOAA,Department of Earth and Environmental Sciences
[18] GEOMAR Helmholtz Centre for Ocean Research,NCAS
[19] National Taiwan University,Climate
[20] Utah State University,Department of Oceanography
[21] Centro de Estudios Avanzado en Zonas Áridas (CEAZA),School of Urban and Environmental Engineering
[22] Laboratoire d’Etudes en Géophysique et Océanographie Spatiale,Climate Prediction Department
[23] Monash University,Laboratory for Climate Studies, National Climate Center
[24] University of Mary Washington,ARC Centre of Excellence for Climate System Science, Faculty of Science
[25] Laboratoire d’Océanographie et du Climat: Expérimentation et Approches Numériques (LOCEAN),Institute of Oceanology
[26] IRD/UPMC/CNRS/MNHN,Department of Marine Sciences and Convergent Technology
[27] University of Reading,School of Earth Sciences and Environmental Engineering
[28] Chonnam National University,undefined
[29] Met Office Hadley Centre,undefined
[30] Ulsan National Institute of Science and Technology,undefined
[31] APEC Climate Center,undefined
[32] Australian Bureau of Meteorology,undefined
[33] China Meteorological Administration,undefined
[34] University of New South Wales,undefined
[35] Instituto Geofisico del Peru,undefined
[36] University of Exeter College of Engineering,undefined
[37] Mathematics and Physical Sciences,undefined
[38] Chinese Academy of Sciences,undefined
[39] Hanyang University,undefined
[40] Gwangju Institute of Science and Technology,undefined
[41] CSIRO Ocean and Atmosphere,undefined
来源
Nature | 2018年 / 559卷
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摘要
El Niño events are characterized by surface warming of the tropical Pacific Ocean and weakening of equatorial trade winds that occur every few years. Such conditions are accompanied by changes in atmospheric and oceanic circulation, affecting global climate, marine and terrestrial ecosystems, fisheries and human activities. The alternation of warm El Niño and cold La Niña conditions, referred to as the El Niño–Southern Oscillation (ENSO), represents the strongest year-to-year fluctuation of the global climate system. Here we provide a synopsis of our current understanding of the spatio-temporal complexity of this important climate mode and its influence on the Earth system.
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页码:535 / 545
页数:10
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