
Numerical simulations uncover a mechanism that consistently explains changes in extreme El Niño events in response to past and future climate forcings, which is supported by paleoclimate data.


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A combination of palaeoclimate proxies and simulations shows that a common mechanism controls El Niño variation in cold and warm states, which supports expectations of more extreme El Niño&nbsp;occurrence in the future.

Future increase in extreme El Niño supported by past glacial changes - Nature

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Numerical Simulations Reveal Mechanism Linking Past Glacial Changes to Increased Likelihood of Extreme El Niño Events in the Future
