The teleconnection between the Atlantic Niño and the Pacifc El Niño Southern Oscillation (ENSO) is revisited using observational and reanalysis data for the 1905–2014 period. Two types of Atlantic Niño are signifcantly negatively correlated with ENSO, with Atlantic leading ENSO by 6-month to 1-year. The frst one is the already well-known connection between the boreal summer Atlantic Niño (ATL3: 3° N–3° S, 20° W...
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