El Niño and La Niña refer to opposite phases of the El Niño-Southern Oscillation (ENSO) cycle in the Pacific Ocean and atmosphere. El Niño occurs when warmer than average sea surface temperatures develop in the eastern tropical Pacific, while La Niña has cooler than average temperatures. These phases influence weather patterns around the world. During a strong El Niño, southern California typically sees more powerful storms and higher rainfall, while a La Niña often brings extremely dry conditions to the region.