Science1 publisherNot yet confirmed elsewhere3 min readPublished
Record-strength El Niño may leave behind climate shifts lasting decades
This El Niño is already the strongest on record, running 3.4C above average in an equatorial Pacific region and still climbing, New Scientist reports. The larger worry is climate regime shifts that could persist for decades after the Pacific cools.
The Scientist · Science desk

What happened
- Forecasts have the event strengthening further before it peaks around November or December.
- Combined model forecasts put the end by June next year, though some individual models keep it going well into the northern summer.
- The two recent strong analogues ended differently: 1997 dropped 8C in a month into a long La Niña, while 2015 faded into a weak, short one.
- Gulf of Mexico sea temperatures jumped after the 2015 super El Niño and stayed high, a rise Seoul National University's Jong-Seong Kug says El Niño helped cause but not alone.
- New Scientist expects this El Niño to bring a devastating Amazon drought that could kill some of the remaining rainforest.
Compiled by The ScientistSomething wrong?How this is made
Why it matters
- exposure An Amazon loss would not reverse when the Pacific cools: dead forest stops supplying the evaporation behind much of the region's rain, and its carbon goes into the air.
- constraint Any relief in 2028 depends on a La Niña soaking up extra heat, and the two strong precedents produced opposite La Niñas, so that relief cannot be planned from history.
- decision Flood planning near the Indian Ocean has to run past the forecast June end, since that ocean tends to warm after El Niños; the 1998 Yangtze floods came after the event ended in May.
The record is set in one patch of ocean. An El Niño is declared when sea-surface temperature in a region along the equator runs 0.5C above average [2], so the current reading is 6.8 times that bar [20]. The warmth starts in the western Pacific, where warm water builds up and then spills east across the equator [3].
Ending one takes several processes working at once. The warm water slowly disperses, partly by flowing away from the equator, and it cools as it hands vast amounts of heat to the atmosphere. That handover produces the sudden jump in global surface temperatures [6]. Below the surface, warm water arriving in the east sets off Rossby waves that travel west [7]. Months later they hit the western continental shelf and bounce back east as faster, cold Kelvin waves [7]. When those arrive weeks after that, they thin the warm layer and let deeper, colder water reach the surface [7].
"Many different processes are involved in the onset, maturation and demise of El Niño events," said Michael McPhaden of the US National Oceanic and Atmospheric Administration [8]. Those processes did not line up the same way in the last two strong events [9]. "So, at this point, it is difficult to know precisely how the current El Niño will wind down," he said [10]. "Nature loves to confound us with new wrinkles in the epic saga of El Niño, so be prepared for surprises." [11]
Jeff Masters, a hurricane specialist, expects the effects to outlast the event. "I expect that this super El Niño event will drive multiple climate regime shifts like we've seen after past super El Niño events," he said [5]. Jong-Seong Kug at Seoul National University and colleagues published a study last year showing that extreme El Niños combined with global warming can produce such shifts [13]. According to New Scientist, the stronger event now under way is more likely to trigger them [19]. "We are experiencing a very strong El Niño event," Kug said [15].
The thing this evidence does not tell you is how much of any one shift belongs to the El Niño. The named precedents are two events, 1997 and 2015 [9]. In the documented case, the Gulf of Mexico, Kug said the 2015 El Niño contributed but was not the only factor [14]. A step change that follows an event and then persists is consistent with a trigger. One case cannot separate the El Niño's push from the warming trend underneath it. The Amazon outlook is less tested still, since New Scientist states it as an expectation [16].
Part of the heat shows up in the global average [6]. This year is on track to tie 2024 at about 1.6C above the pre-industrial level, and 2027 is expected to reach 1.7C or more [17]. By New Scientist's reckoning, the world is on the brink of permanently crossing the 1.5C threshold it was meant to avoid [18].
What to watch
- Whether the equatorial reading keeps climbing past 3.4C toward the forecast November-December peak.
- Which way the event ends: a 1997-style collapse into a strong La Niña or a 2015-style fade, and whether the models that keep it running into the northern summer are right.
- Field measurements of Amazon rainfall and tree die-off during the drought New Scientist expects, the first direct test of the permanent-drying claim.
Clarity's read
What the record supports and how the coverage leans. The claims behind it follow.
Reality
- Evidence50
- Adoption
- Insufficient
- Hype gap+25
- Incentives
- Insufficient
- Confidence55
Claim ledger
Ranked by verification strength, evidence, and original report placement.
- [1]
The current El Niño is already the strongest on record and is forecast to get even stronger, peaking around November or December.
- [2]
An El Niño is said to be happening when the sea-surface temperature in one region along the equator is 0.5C above average; at the time of writing it was 3.4C and climbing.
- [3]
El Niños occur when warm water that has built up in the western Pacific spills east across the equator, making the surface of the eastern Pacific warmer than usual.
- [4]
The combined forecasts of computer models suggest this El Niño will be over by June next year, but individual models vary and some suggest it could persist well into the northern hemisphere's summer.
- [5]
"I expect that this super El Niño event will drive multiple climate regime shifts like we've seen after past super El Niño events."
ReportedSupportedSource: Jeff Masters, hurricane specialist, quoted by New ScientistView cited source - [6]
El Niños end partly because the warm water slowly disperses, some flowing away from the equator, and cools as it transfers vast amounts of heat to the atmosphere, which leads to a sudden jump in global surface temperatures.
- [7]
Warm water arriving in the eastern Pacific triggers westward-travelling Rossby waves; months later these hit the western Pacific continental shelf and bounce back east as cold, faster Kelvin waves, which several weeks later thin the warm layer in the eastern Pacific and help deeper, colder water reach the surface.
- [8]
"Many different processes are involved in the onset, maturation and demise of El Niño events."
ReportedSupportedSource: Michael McPhaden, US National Oceanic and Atmospheric Administration, quoted by New ScientistView cited source - [9]
The 1997 El Niño ended with eastern equatorial Pacific sea-surface temperatures plummeting by 8C in a month, followed by a strong, long-lasting La Niña; the next strong El Niño, in 2015, faded gradually and was followed by a weak, short La Niña.
- [10]
"So, at this point, it is difficult to know precisely how the current El Niño will wind down."
- [11]
"Nature loves to confound us with new wrinkles in the epic saga of El Niño, so be prepared for surprises."
- [12]
The Indian Ocean can become warmer after El Niños, on top of warming from global heating, leading to floods in some nearby regions; some of the worst Yangtze river floods occurred in summer 1998, after the El Niño that ended in May.
- [13]
Last year Jong-Seong Kug at Seoul National University and colleagues published a study showing that the combination of extreme El Niños and global warming can produce climate regime shifts.
- [14]
After the 2015 super El Niño there was a sudden increase in Gulf of Mexico sea-surface temperatures that has persisted since; Kug says the El Niño was not the only factor but contributed to the jump.
- [15]
"We are experiencing a very strong El Niño event."
- [16]
This El Niño is expected to lead to a devastating Amazon drought that could kill off some of the remaining rainforest, releasing huge quantities of carbon dioxide and making the region permanently drier, because much of the rainfall in rainforests comes from water evaporating from trees.
- [17]
This year's average temperature is on track to tie with 2024's at around 1.6C above the pre-industrial level, and 2027 is expected to reach 1.7C or more.
- [18]
The year after 2027 could be a bit cooler if a La Niña makes the Pacific soak up more heat than usual, but the world is on the brink of permanently crossing the 1.5C threshold it was meant to avoid.
- [19]
The biggest concern is that the current El Niño could lead to changes that last decades or more; the even-stronger El Niño now under way is more likely to trigger such regime shifts.
- [20]
The current equatorial reading of 3.4C above average is 6.8 times the 0.5C threshold that defines an El Niño.
Sources
1 independent publisher whose own reporting we read for this story.
- newscientist.comThe world may never go back to how it was after this monster El Niño
1 article · October 8, 2026
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Entities
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