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Deep beneath the surface of the equatorial Pacific Ocean, an immense reservoir of heat is moving eastward, destabilizing the global climate system with a speed that has caught researchers off guard.
Just months after a weak La Niña cooling phase faded into a brief period of atmospheric neutrality, the tropical Pacific is warming at an extraordinary rate. On Thursday, the National Oceanic and Atmospheric Administration (NOAA) issued an updated climate outlook, reporting an 82 percent chance that a full-blown El Niño will establish itself by July, with a near-certain 96 percent probability of persisting through the Northern Hemisphere winter.
But it is the potential intensity of this event, rather than its mere arrival, that is triggering alarms in climate research hubs from Tokyo to Exeter.
Computer models are increasingly aligned on a rare, high-consequence scenario: ocean surface temperatures in the central Pacific could soar to 2 degrees Celsius (3.6 degrees Fahrenheit) or more above the historical baseline. While agencies like the British Met Office and the World Meteorological Organization avoid the unscientific phrasing, the broader meteorological community has begun using a more ominous moniker to describe an event of this magnitude: a “Super El Niño.”
“The transition from a cooling state to extreme warming has been remarkably swift,” said Kris Karnauskas, a climate scientist and associate professor at the University of Colorado Boulder. “It starts with the ocean, but it has a profound ripple effect on weather all over the world. It locks the atmosphere into a persistent, high-energy pattern for months on end.”

An El Niño is a naturally occurring phenomenon characterized by a weakening of the trade winds that normally push warm water toward Asia. When those winds slacken or reverse, the warm water sloshes backward toward South America, fundamentally altering the jet streams that dictate where storms form and where droughts linger.
If the current projections hold true—with some European models estimating that specific zones of the Pacific could hit an astonishing 3 degrees Celsius above average by November—this event would enter the upper echelon of climate anomalies. Scientists are already drawing comparisons to the devastating 1997–1998 and 2015–2016 episodes, the latter of which was memorably dubbed the “Godzilla El Niño.”
PROJECTED GLOBAL SEA-SURFACE TEMPERATURE ANOMALIES (FALL 2026)
Normal Baseline ....................... 0.0°C
Standard El Niño Threshold ............ +0.5°C
Moderate Event ........................ +1.0°C to +1.5°C
"Super El Niño" Projection ............ +2.0°C to +3.0°C
“Some researchers are telling us this could be the strongest El Niño event of the century so far,” said Grahame Madge, a senior press officer and climate science communicator at the UK Met Office.
However, the 2026 iteration comes with a dangerous catch. Unlike the great El Niños of the 20th century, this one is superimposing itself onto an ocean and atmosphere already severely heated by greenhouse gas emissions. The structural baseline of global temperatures has risen so significantly that even the cool La Niña years of the 2020s were warmer than the strong El Niño years of the late 1990s.
“El Niño doesn’t create heat out of nowhere; it discharges heat from the ocean into the atmosphere,” Dr. Karnauskas explained. “When you dump that volume of thermal energy into an already overloaded system, the impacts are amplified. It provides unprecedented moisture and energy for extreme weather.”
The human and economic costs of a Super El Niño are traditionally measured in billions of dollars and widespread agricultural disruption. Because the Pacific Ocean is the planet’s largest heat engine, its shifts dictate a starkly divided geography of climate misery.
In Latin America, humanitarian organizations are already mobilizing. According to the International Federation of Red Cross and Red Crescent Societies (IFRC), a severe warming event threatens to plunge the Central American Dry Corridor into prolonged, severe droughts, decimating traditional agricultural cycles and threatening food security. Conversely, the “Southern Cone”—including parts of Uruguay, southern Brazil, and central Chile—must brace for torrential, flood-inducing rainfall.
EXPECTED REGIONAL IMPACTS OF A POWERFUL EL NIÑO
Wetter-Than-Average Drier-Than-Average
----------------------------------- ----------------------------------
• Southern United States / California • Eastern Australia
• Horn of Africa • Indonesia & Southeast Asia
• Southern Cone of South America • Northern Brazil & Colombia
• Central Asia • Indian Monsoon Region
For the United States, a potent winter El Niño typically brings a split personality to the weather map. It generally ushers in wetter, cooler conditions across the southern tier of the country—from California through the Southwest to the Gulf Coast—frequently shifting major storm tracks southward.
The phenomenon also has a dramatic effect on the tropical storm seasons. In the Atlantic, El Niño historically increases vertical wind shear—essentially tearing storms apart before they can organize—which could suppress hurricane development. But in the Pacific, the hyper-warmed waters provide raw fuel, potentially yielding an unusually active and dangerous season for powerful typhoons.

While the immediate atmospheric chaos will likely peak between November 2026 and February 2027, meteorologists are looking even further down the calendar with deep concern.
Because of the lag time required for the ocean’s released heat to fully mix into the global atmosphere, the second year of a major El Niño is almost always the hottest. The combination of the 2023 El Niño and human-caused warming made 2024 the warmest year on record.
If the current event reaches the “Super” threshold by the end of this year, scientists warn that 2027 is virtually locked in to smash global temperature records, potentially pushing the planet, if temporarily, past the critical 1.5 degrees Celsius threshold of warming above pre-industrial levels.
For now, the scientific community is watching the data roll in from deep-sea buoys and orbital satellites, navigating what meteorologists call the “spring predictability barrier”—a window in April and May where long-range models are notoriously fickle.
“We still have a few weeks before we know for certain if the ocean-atmosphere coupling will lock in perfectly over the summer,” said NOAA’s Climate Prediction Center in a cautious addendum to its report. “A stronger El Niño makes these extreme impacts more likely, but it doesn’t guarantee them. The atmosphere always keeps us guessing.”