<p>The sea surface temperature (SST), anomalies (SST), ONI (Oceanographic El Niño Index) and MEI (Multivariate ENSO Index) in regions El Niño 1 + 2 (80° W–90° W, 0°–10° S) and 3.4 (5° N–5° S, 170° W–120° W) as well as the Pacific Decadal Oscillation (PDO) and Atlantic Multidecadal Oscillation (AMO) indexes were correlated to sun spots number (SS) from cycles (SS#) 19 to 24 (1954–2017). Degree-six polynomial regression functions represented each of the six cycles with an average r<sup>2</sup> > 0.89 (p < 0.001). The series of correlations at different lag times (0, 6, 12, 24, 36 and 48 months) gave a response time: 12–36 months. In the 1954–2017 period, the whole series of SS cycles did not show a strong correlation with the variables and SST Anomaly in the El Niño areas 1 + 2 and 3.4. The highest correlations r<sup>2</sup> were up to: 0.043, 0.029, 0.040 and 0.021 for PDO, MEI, ONI and SST Anomaly (in 3.4) respectively, suggesting that there is still a correlation with high confidence (p ≤ 0.01). Analysing for the period 1990–2016, the correlations improved up to 0.11, 0.12, and 0.17 for ONI, SST (in 3.4) and PDO correspondingly. The SST correlations against individual SS cycles in regions 3.4 and 1 + 2 were up to 0.219 (SS# 23) and < 0.0675 (SS# 19) correspondingly. SST Anomaly, ONI and MEI correlated with r<sup>2</sup> of 0.250, 0.3943 and 0.2510, one-to-one; the lag time was 24–48 months and linear curves had positive slope. In general, in 1 + 2 there was found a more inconstant and lower correlation than in 3.4 (where also MEI and ONI are measured). On the longer time scales, the PDO (alike AMO) seemed to respond in 36–48 months to SS cycles showing a high degree of correlation coefficient r<sup>2</sup> of 0.625 (SS# 19) and 0.766 (SS# 24); whilst AMO index gave up to 0.490 (SS# 20) with similar lag time. Cycles 19 and 24 showed a better correlation in general. During the ascending phases of each cycle the SST in region 1 + 2 rendered correlation coefficient r<sup>2</sup> and p-value from 0.205 and 0.0008 (SS# 23) to 0.163 and ≤ 0.0044 (SS# 19). In the region 3.4, r<sup>2</sup> were from 0.870 (SS# 24), to 0.556 (SS# 23). In each SS cycle lag time was around 36 months; all of them occurred at the ascending phase, except in cycles 20 and 24. SST anomaly registered r<sup>2</sup> from 0.662 to 0.254 in the ascending phase with a response time 0-48 months and positive linear regression slope (except SS# 23). On the other hand, the descending phase showed a predominantly lower r<sup>2</sup>: < 0.14 (p < 0.01). The region 3.4 had better r<sup>2</sup> than in 1 + 2, from 0.897 (SS# 24) to 0.239 (SS# 21) respectively in the ascending phase except cycles 20 and 24. The lag time was consistent at 36 months. The highest r<sup>2</sup> of 0.897 at the end of the SS# 24 peak, coincided with one of the strongest El Niño (2014–2015) and the second highest r2 (SS# 22 ascending phase) with two consecutive strong El Niño 1991–1995. ONI and MEI also showed strong correlation; the three highest r<sup>2</sup> matched dates of strong El Niño 1987–1989, 1955–1957 and 1997–1998 in the ascending phase. During the descending phases, the correlation coefficients were lower, and ranged from 0.6082 to 0.2938; but with a lag time 0–12 months, and positive slope. The index MEI, as with ONI, registered r<sup>2</sup> lower during descending phases. The PDOs were linearly correlated from 0.7677 to 0.2855 (12 to 24 months) and 0.3522 during ascending and descending phases respectively. On the other hand, r<sup>2</sup> for AMO was up to 0.700. The strength of the linear correlations substantially increased when the ascending and descending phase of each cycle was analysed. During the ascending phase there is a stronger correlation than in the descending phase. These results would indicate that warm events tend to occur in the ascending phase or at the top of the cycle and have a delay time of around 36 months, whilst cold events are associated to a descending phase but with a quicker response time. The sun spot activity should be considered as a factor that could condition and trigger low (PDO and AMO) and high (ONI-El Niño) frequency oceanographic events in the Pacific and Atlantic Oceans. During 2019, the cycle 25 should start, then according to this work probably the next El Niño event would be around 2020–2021 or later.</p>