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Given that ToE is determined by the extent to which the signal of SST variability change exceeds the level of noise, we compare the role of signal and noise in controlling the inter-model differences of ToE. You can also search for this author in PubMed Google Scholar. Previous studies suggested that a warming-induced enhancement of ocean stratification featuring faster warming in the upper-ocean than that below contributes to an increase in EP-ENSO SST variability by boosting the dynamical coupling between ocean and atmosphere in a warming climate

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