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What is El Niño Labelling and Why It Matters for Climate Forecasting

Context

  • National Oceanic and Atmospheric Administration (NOAA) has updated how El Niño and La Niña are officially classified — reflecting a warming world where old baselines no longer apply.

ENSO: The Natural Climate Engine

What Is ENSO?

●     El Niño and La Niña are phases of the El Niño–Southern Oscillation (ENSO) — a recurring climate pattern in the equatorial Pacific Ocean.

○     El Niño occurs when surface waters in the central and eastern Pacific become warmer than normal.

○     La Niña occurs when those waters become cooler than normal.

●     This cycle typically shifts every 2–7 years and influences global weather systems, including rainfall patterns, droughts, cyclones, and heatwaves.

How ENSO Affects Global Temperatures

●     El Niño years usually raise global average temperatures temporarily because warm ocean water releases more heat into the atmosphere.

●     La Niña years slightly cool global temperatures by keeping more heat stored in deeper ocean layers.

●     However, in today’s world, even La Niña phases are occurring on a much warmer background temperature than decades ago.

Why Scientists Changed El Niño Labelling

The Problem with Old Definitions:

  • ENSO events are classified based on how much Pacific Ocean temperatures deviate from a long-term average.
  • But global warming has raised overall ocean temperatures. This means the “normal” baseline used in past decades no longer reflects today’s reality.

NOAA’s Updated Calculation: NOAA revised its system for defining El Niño and La Niña by adjusting the temperature baseline. This recalibration means:

  • Some past El Niño events might not qualify under new criteria.
  • More events may be classified as La Niña.
  • Temperature anomalies are measured relative to a warmer reference period.

In simple terms, the climate has changed so much that scientists had to reset the measuring scale.


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