@article{fdi:010079960, title = {{ENSO} diversity driving low-frequency change in mesoscale activity off {P}eru and {C}hile}, author = {{C}onejero, {C}. and {D}ewitte, {B}oris and {G}arcon, {V}. and {S}udre, {J}. and {M}ontes, {I}.}, editor = {}, language = {{ENG}}, abstract = {{T}ransient mesoscale oceanic eddies in {E}astern {B}oundary {U}pwelling {S}ystems are thought to strongly affect key regional scale processes such as ocean heat transport, coastal upwelling and productivity. {U}nderstanding how these can be modulated at low-frequency is thus critical to infer their role in the climate system. {H}ere we use 26 years of satellite altimeter data and regional oceanic modeling to investigate the modulation of eddy kinetic energy ({EKE}) off {P}eru and {C}hile by {ENSO}, the main mode of natural variability in the tropical {P}acific. {W}e show that {EKE} tends to increase during strong {E}astern {P}acific ({EP}) {E}l {N}ino events along the {P}eruvian coast up to northern {C}hile and decreases off central {C}hile, while it is hardly changed during {C}entral {P}acific {E}l {N}ino and {L}a {N}ina events. {H}owever the magnitude of the {EKE} changes during strong {EP} {E}l {N}ino events is not proportional to their strength, with in particular the 1972/1973 {E}l {N}ino event standing out as an extreme event in terms of {EKE} increase off {P}eru reaching an amplitude three times as large as that during the 1997/1998 {E}l {N}ino event, and the 2015/2016 {E}l {N}ino having instead a weak impact on {EKE}. {T}his produces decadal changes in {EKE}, with a similar pattern than that of strong {EP} {E}l {N}ino events, resulting in a significant negative (positive) long-term trend off {P}eru (central {C}hile).}, keywords = {{PACIFIQUE} ; {CHILI} ; {PEROU}}, booktitle = {}, journal = {{S}cientific {R}eports - {N}ature}, volume = {10}, numero = {1}, pages = {17902 [73 p.]}, ISSN = {2045-2322}, year = {2020}, DOI = {10.1038/s41598-020-74762-x}, URL = {https://www.documentation.ird.fr/hor/fdi:010079960}, }