1. Introduction to El Niño
Definition:
El Niño is a complex climate phenomenon characterized by the warming of sea surface
temperatures in the central and eastern equatorial Pacific Ocean. This event disrupts normal
weather patterns around the globe, occurring irregularly every 2 to 7 years.
El Niño Southern Oscillation (ENSO): El Niño is part of a broader climate cycle known as
ENSO, which includes its opposite phase, La Niña, associated with cooler ocean
temperatures. ENSO has three phases: El Niño (warm phase), La Niña (cool phase), and a
neutral phase.
Origins:
The name "El Niño" comes from Spanish, meaning "The Child," as early Peruvian fishermen
noticed the event typically occurred around Christmas.
Key Features of El Niño:
Warming of 0.5°C or more in sea surface temperatures in the central/eastern Pacific.
Weakening or reversal of trade winds that normally blow from east to west.
Occurrence typically around the end of the year, lasting 9–12 months.
2. Mechanics of El Niño: How Does it Work?
Normal Conditions vs. El Niño Conditions:
Normal Conditions:
Under typical conditions, trade winds blow from east to west across the equatorial Pacific,
pushing warm water towards the western Pacific near Indonesia and Australia. This allows for
upwelling of cold, nutrient-rich water along the coast of South America.