@article{fdi:010073701, title = {{E}l {N}ino-{S}outhern {O}scillation complexity}, author = {{T}immermann, {A}. and {A}n, {S}. {I}. and {K}ug, {J}. {S}. and {J}in, {F}. {F}. and {C}ai, {W}. {J}. and {C}apotondi, {A}. and {C}obb, {K}. and {L}engaigne, {M}atthieu and {M}c{P}haden, {M}. {J}. and {S}tuecker, {M}. {F}. and {S}tein, {K}. and {W}ittenberg, {A}. {T}. and {Y}un, {K}. {S}. and {B}ayr, {T}. and {C}hen, {H}. {C}. and {C}hikamoto, {Y}. and {D}ewitte, {B}oris and {D}ommenget, {D}. and {G}rothe, {P}. and {G}uilyardi, {E}. and {H}am, {Y}. {G}. and {H}ayashi, {M}. and {I}neson, {S}. and {K}ang, {D}. and {K}im, {S}. and {K}im, {W}. and {L}ee, {J}. {Y}. and {L}i, {T}. and {L}uo, {J}. {J}. and {M}c{G}regor, {S}. and {P}lanton, {Y}. and {P}ower, {S}. and {R}ashid, {H}. and {R}en, {H}. {L}. and {S}antoso, {A}. and {T}akahashi, {K}. and {T}odd, {A}. and {W}ang, {G}. {M}. and {W}ang, {G}. {J}. and {X}ie, {R}. {H}. and {Y}ang, {W}. {H}. and {Y}eh, {S}. {W}. and {Y}oon, {J}. and {Z}eller, {E}. and {Z}hang, {X}. {B}.}, editor = {}, language = {{ENG}}, abstract = {{E}l {N}ino events are characterized by surface warming of the tropical {P}acific {O}cean and weakening of equatorial trade winds that occur every few years. {S}uch conditions are accompanied by changes in atmospheric and oceanic circulation, affecting global climate, marine and terrestrial ecosystems, fisheries and human activities. {T}he alternation of warm {E}l {N}ino and cold {L}a {N}ina conditions, referred to as the {E}l {N}ino-{S}outhern {O}scillation ({ENSO}), represents the strongest year-to-year fluctuation of the global climate system. {H}ere we provide a synopsis of our current understanding of the spatio-temporal complexity of this important climate mode and its influence on the {E}arth system.}, keywords = {{PACIFIQUE}}, booktitle = {}, journal = {{N}ature}, volume = {559}, numero = {7715}, pages = {535--545}, ISSN = {0028-0836}, year = {2018}, DOI = {10.1038/s41586-018-0252-6}, URL = {https://www.documentation.ird.fr/hor/fdi:010073701}, }