The relationship between the duration of El Niño events and the timing of subsequent occurrences remains complex and not fully understood. El Niño events are characterized by significant sea-surface warming in the eastern equatorial Pacific, driven primarily by solar heating, with ocean currents playing a role in redistributing this heat rather than generating it. The phenomenon is influenced by a combination of atmospheric and oceanic factors, with oscillations between El Niño and La Niña events indicating a dynamic ocean-atmosphere system. During El Niño, warm water moves eastward along the equator due to Kelvin waves, while La Niña conditions confine warm waters to the west, enhancing upwelling and nutrient availability along the American coast. The chaotic nature of these events suggests non-linear interactions within the coupled ocean-atmosphere system, where perturbations can originate from either the ocean or the atmosphere. Additionally, the removal of cold water can theoretically lead to increased sea temperatures, highlighting the significant role of ocean currents in climate dynamics.