El Niño/Southern Oscillation
Quick Summary
The El Niño/Southern Oscillation (ENSO) is a climate pattern characterized by fluctuations in sea surface temperatures and atmospheric pressure across the tropical Pacific Ocean. It has two main phases: El Niño, marked by warmer-than-normal sea surface temperatures in the eastern Pacific, and La Niña, characterized by cooler-than-normal temperatures.1234
These shifts in ocean temperatures influence global weather patterns, leading to varied effects such as droughts in some regions and increased rainfall in others. ENSO events occur irregularly, typically every two to seven years, and can have significant impacts on ecosystems, agriculture, and weather worldwide.124
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