The influence NATV → ENSO is explained in 9 , 16 as being due to triggering of the El Niño events by the north tropical Atlantic via the Atlantic and Pacific intertropical convergence zones, which equally applies to the present work where the influence NATV → ENSO is also found to be quite significant and sometimes even stronger than the opposite one.
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Contribution of North Atlantic temperature variability to El Niño cyclicity as revealed by spectral causality estimates.
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