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What is a super El Niño and how does it affect global weather records?

A super El Niño is just an unusually strong El Niño, and the 2026–2027 event has been labeled very strong and is expected to peak late in the year.

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Covers: This page explains what a super El Niño is, how it differs from a typical El Niño, and how it influences global temperature and precipitation records. It covers the physical mechanisms and observed impacts, not local forecasts or climate change attribution debates.

Also answers: What is a super El Niño? · Super El Niño meaning and effects · How does a super El Niño affect weather? · Super El Niño vs regular El Niño

The short answer

Evidence-backed AI-prepared starting map

A "super El Niño" is an informal label for an exceptionally strong El Niño — the warming phase of ENSO, the coupled ocean-atmosphere phenomenon of the tropical Pacific. The ongoing 2026–2027 event was declared on 2 June 2026 by the World Meteorological Organization, is described as the strongest El Niño ever measured for its time of year, has already been…12

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At a glance

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The evidence behind it

6 sources
  • Other studies and data3
  • Background3

Published in 2025 and 2026

Sources on this page by kind and year
SourceKindYear
Super El Niño sets another record as it strengthens to 'unprecedented levels'Background2026
2024 global temperature record is consistent with model-predicted warming.Other studies and data2026
An eastward-propagating coupled mode amplifying the early growth of extreme El Niño events.Other studies and data2026
Synergies Between Observed Warming and ENSO Episodes on Extreme Events.Other studies and data2025
El Niño–Southern Oscillation (Wikipedia)BackgroundUnknown
2026–2027 El Niño event (Wikipedia)BackgroundUnknown

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In brief

  1. A super El Niño is an exceptionally strong El Niño; the 2026–2027 event has been classified as a "very strong El Niño" and is expected to peak in November or December.1

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  2. El Niño is the warm phase of ENSO, typically lasting about a year and recurring every two to seven years with varying intensity.2

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  3. Extreme El Niño events share an early, reproducible precursor: an eastward-propagating coupled mode in the western-central equatorial Pacific with sustained westerly winds, detectable as early as February.3

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  4. El Niño-boosted years dominate recent global temperature records: 2024 had about a 12% likelihood and 2016 about 14%, while only 1998 was truly anomalous at about 2.5% — and all were nearly impossible without human-caused warming.4

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  5. Warming has amplified ENSO's effects on temperature and precipitation extremes worldwide and shifted their spatial patterns, raising risk for large shares of population, GDP, agriculture and ecosystems.5

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What it means for you

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If you want to know whether a strong El Niño is developing

watch for the early precursor described in the research: a slow eastward-propagating coupled mode in the western-central equatorial Pacific during boreal winter and spring, with warm sea surface temperatures and sustained westerly winds, which has allowed skillful forecasts of extreme events as early as February.3

Evidence-backed

If you are tracking global temperature records

expect El Niño years to raise the odds of a record: the El Niño-boosted 2024 record had about a 12% likelihood and 2016 about 14%, versus about 2.5% for 1998, and each was nearly impossible without human-caused warming.4

Evidence-backed

If you are assessing risk from temperature and precipitation extremes

account for the interaction between warming and ENSO, which has amplified ENSO's effects on extremes worldwide and modified their spatial patterns, putting considerable shares of population, GDP, agriculture and ecosystems at higher risk.5

Evidence-backed

If you are following the 2026–2027 event

note that onset was declared on 2 June 2026, it is the strongest El Niño measured for its time of year, and it is expected to peak in November or December and last through early 2027 — the point at which record comparisons become most testable.1

Evidence-backed

If you need a working definition of El Niño itself

treat it as the warm phase of ENSO, the coupled ocean-atmosphere phenomenon of the tropical Pacific, typically lasting about a year and recurring every two to seven years with varying intensity.2

Evidence-backed

The full explanation

Evidence-backed AI-prepared starting map

A "super El Niño" is an informal label for an exceptionally strong El Niño — the warming phase of ENSO, the coupled ocean-atmosphere phenomenon of the tropical Pacific. The ongoing 2026–2027 event was declared on 2 June 2026 by the World Meteorological Organization, is described as the strongest El Niño ever measured for its time of year, has already been classified as a "very strong El Niño" (also called a Super El Niño), and is expected to peak in November or December and last through early 2027. El Niño events typically last about a year and recur every two to seven years with varying intensity.12

What this rests on6 independent sources
  • Evidence 19
  • Interpretation 3

The full story · 4 chapters

01

What a super El Niño is, and how it differs from a typical El Niño

AI summary:El Niño is the warm phase of ENSO, and a super El Niño is simply its strongest end, as in the 2026–2027 event.

Evidence-backed

Evidence-backed: ENSO is a global climate phenomenon arising from variations in winds and sea surface temperatures over the tropical Pacific. Its warm phase is El Niño and its cool phase is La Niña, with an accompanying atmospheric oscillation (the Southern Oscillation) coupled to the sea temperature change. Events typically last about one year and occur every two to seven years with varying intensity, separated by weaker neutral periods. El Niño is associated with higher-than-normal sea level air pressure over Indonesia, Australia and across the Indian Ocean to the Atlantic; La Niña roughly reverses that pattern.2

Evidence-backed

Evidence-backed: A super El Niño is the strong end of that range rather than a separate phenomenon. The 2026–2027 event has been classified as a "very strong El Niño", also known as a Super El Niño, and the WMO has reported it will likely be the strongest El Niño on record. It is already the strongest El Niño ever measured for its time of year, and is expected to peak in November or December before lasting through early 2027.1

Interpretation

Interpretation: The practical difference between a typical and an extreme El Niño is not just peak warmth but how early and how reproducibly the event can be anticipated. Extreme events are among the most consequential climate phenomena, yet their early prediction has long been difficult.3

02

The physical mechanism: an early coupled precursor

AI summary:Extreme El Niños share an early, reproducible ocean-atmosphere precursor that can allow forecasts as early as February.

Evidence-backed

Evidence-backed: Analysis of the 1982/1983, 1997/1998 and 2015/2016 events, together with a large ensemble of climate model simulations, identifies an unusually early and reproducible ocean-atmosphere precursor to extreme El Niño: a slow, eastward-propagating coupled mode that develops in the western-central equatorial Pacific during boreal winter and spring. It features warm sea surface temperature anomalies coupled with sustained westerly wind anomalies. Those westerly winds drive equatorward transport of warm water, rapidly raising equatorial ocean heat content and priming extreme El Niño growth in the following summer and fall.3

Evidence-backed

Evidence-backed: Ensemble hindcasts indicate that East Asian cold surges and the North Pacific Oscillation can stochastically excite this equatorial mode, which allows skillful forecasts of extreme events as early as February and helps overcome the spring predictability barrier. In other words, the same mechanism that makes these events extreme also makes them, in principle, detectable earlier than a typical El Niño.3

03

How it shows up in global temperature and precipitation records

AI summary:El Niño-boosted years dominate recent global temperature records, and warming has amplified ENSO's effects on extremes worldwide.

Evidence-backed

Evidence-backed: El Niño-boosted years are prominent in the global temperature record. A semiempirical assessment combining climate model simulations with observed temperatures found that the El Niño-boosted 2024 global temperature record had roughly a 12% likelihood of occurrence — about a one-in-eight-year event — similar to the prior, also El Niño-boosted, record year 2016 at about 14%. Of the records set over the past three decades, only 1998 was found to be truly anomalous, with about a 2.5% likelihood. Each of these records was found to be nearly impossible without human-caused warming.4

Evidence-backed

Evidence-backed: On precipitation and extremes, current warming has amplified the effects of ENSO on temperature and precipitation extremes worldwide, and has extensively modified their spatial patterns. Considerable shares of population, GDP, agriculture and ecosystems now face higher risk from extreme events because of the interaction between increased anthropogenic forcing and ENSO. Past events illustrate the severe societal consequences of the phenomenon through weather disasters, food security, health, economic growth, migration and conflict.5

Interpretation

Interpretation: Read together, these results suggest that a super El Niño matters for records in two ways: it raises the odds that a given year sets a global temperature record, and it shifts the geography and severity of temperature and precipitation extremes. The temperature-record evidence is quantitative; the extreme-event amplification is described in directional terms, so the size of the effect on any particular region is not pinned down by these sources.45

04

The live case: 2026–2027

AI summary:The 2026–2027 El Niño was declared in June 2026, is called very strong, and is expected to peak in November or December.

Evidence-backed

Evidence-backed: The 2026–2027 El Niño had its onset declared on 2 June 2026 by the WMO. It is the strongest El Niño ever measured for its time of year, has been classified as a "very strong El Niño" or Super El Niño, and the WMO has reported it will likely be the strongest El Niño on record. It is expected to peak in November or December and to last through early 2027.1

Evidence-backed

Evidence-backed: Reporting on the event notes that El Niño has continued to strengthen, with several key measures now in record territory, and compares it with previous events.6

Interpretation

Interpretation: Because the event is still unfolding, the "strongest on record" framing is a projection rather than a settled measurement; the peak months are the point at which the comparison with 1982/1983, 1997/1998 and 2015/2016 will be most directly testable.13

Before you go

What to remember

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  1. A super El Niño is an exceptionally strong El Niño; the event has been classified as a "very strong El Niño" and is expected to peak in November or December.

  2. El Niño-boosted years dominate recent global temperature records: 2024 had about a likelihood and 2016 about 14%, while only 1998 was truly anomalous at about 2.5% — and all were nearly impossible without human-caused warming.

  3. El Niño is the warm phase of ENSO, typically lasting about a year and recurring every two to seven years with varying intensity.

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  1. 1
    2026–2027 El Niño event (Wikipedia)
    WikipediaPublished Oct 14, 2026Checked Oct 14, 2026
    “The 2026–2027 El Niño is the ongoing El Niño event, with its onset declared on 2 June 2026 by the World Meteorological Organization (WMO). It is the strongest El Niño ever measured for its time of year, and the World Meteorological Organization has reported that it will likely be the strongest El Niño on record, with it already being classified as a "very strong El Niño", also known as a Super El Niño. The 2026–2027 El Niño is expected to peak in November or December and last through early 2027.”
  2. 2
    El Niño–Southern Oscillation (Wikipedia)
    WikipediaPublished Oct 14, 2026Checked Oct 14, 2026
    “El Niño–Southern Oscillation (ENSO) is a global climate phenomenon that emerges from variation in winds and sea surface temperatures over the tropical Pacific Ocean. Those variations have an irregular pattern, but do have some appearance of cycles. The occurrence of ENSO is not easily predictable. It affects the climate of much of the tropics and subtropics, and has links (teleconnections) to higher-latitude regions of the world. The warming phase of the sea surface temperature is known as "El Niño" and the cooling phase as "La Niña". The Southern Oscillation is the accompanying atmospheric oscillation, which is coupled with the sea temperature change. El Niño is associated with higher than normal sea level air pressure over Indonesia and Australia, and across the Indian Ocean to the Atlantic Ocean. La Niña has roughly the reverse pattern: high pressure over the central and eastern Pacific and lower pressure through much of the rest of the tropics and subtropics. The two phenomena typically last approximately one year each and typically occur every two to seven years with varying intensity, with neutral periods of lower intensity interspersed.”
  3. 3
    An eastward-propagating coupled mode amplifying the early growth of extreme El Niño events.
    Science advances (Liang et al.)Published Sep 23, 2026Checked Oct 14, 2026
    “Extreme El Niño events are among the most consequential climate phenomena, yet their early prediction remains challenging. Here, by analyzing the 1982/1983, 1997/1998, and 2015/2016 events together with a large ensemble of climate model simulations, we identify an unusually early and reproducible ocean-atmosphere precursor to extreme El Niño: a slow, eastward-propagating coupled mode that develops in the western-central equatorial Pacific during boreal winter and spring. This mode features warm sea surface temperature anomalies coupled with sustained westerly wind anomalies. These westerly wind anomalies drive the equatorward transport of warm water, rapidly increasing equatorial ocean heat content and priming extreme El Niño growth in the following summer and fall. Ensemble hindcasts further reveal that East Asian cold surges and the North Pacific Oscillation can stochastically excite this equatorial mode, enabling skillful forecasts of extreme events as early as February and helping to overcome the spring predictability barrier.”
  4. 4
    2024 global temperature record is consistent with model-predicted warming.
    Proceedings of the National Academy of Sciences of the United States of America (Mann et al.)Published May 11, 2026Checked Oct 14, 2026
    “We employ a semiempirical approach combining climate model simulations and observational temperatures to assess the likelihood of recent global temperature records. Monte Carlo simulations are used to generate global temperature series consistent with combined estimates of forced (anthropogenic + natural) and internal variability derived from observations and CMIP6 multimodel simulations. We find that the El Niño-boosted 2024 global temperature record had a ~12% likelihood of occurrence (a one-in-eight-year event), similar to the prior (also El Niño-boosted) record year 2016 (~14% likelihood). Of the records set during the past three decades, only 1998 is found to have been truly anomalous, with a ~2.5% likelihood of occurrence. Each of these records is found to have been nearly impossible in the absence of human-caused warming.”
  5. 5
    Synergies Between Observed Warming and ENSO Episodes on Extreme Events.
    Annals of the New York Academy of Sciences (Estrada et al.)Published Nov 4, 2025Checked Oct 14, 2026
    “Past events illustrate the severe societal consequences this phenomenon has through weather disasters, food security, health, economic growth, migration, and conflict. ENSO's interactions with global warming are not well understood, although they can lead to significant changes in the characteristics of extreme events. Climate conditions in 2024/2025 may favor widespread severe extreme events with global temperature anomalies nearing or surpassing 1.5°C and a transition from strong El Niño to La Niña conditions. Here, we show that current warming has amplified the effects of ENSO on temperature and precipitation extremes worldwide. Results show that warming has produced a considerable amplification of the effects of ENSO episodes over such extremes, as well as extensively modified spatial patterns. We show that considerable shares of the population, gross domestic product, agriculture, and ecosystems now face a higher risk from extreme events due to the interactions between increased anthropogenic forcing and ENSO.”
  6. 6
    Super El Niño sets another record as it strengthens to 'unprecedented levels'
    BBC NewsPublished Oct 13, 2026Checked Oct 14, 2026
    “El Niño has continued to strengthen, with several key measures now in record territory. Simon King explores how it compares to previous events.”

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Open questions

  • Is there a formal index threshold that defines a "super" El Niño, or is the term purely descriptive of the strongest events?

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  • How will the 2026–2027 event compare with 1982/1983, 1997/1998 and 2015/2016 once it peaks in November or December?

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  • How much of any 2026 global temperature record would be attributable to this El Niño versus background warming?

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  • Which regions see the largest changes in precipitation extremes during a super El Niño compared with a moderate one?

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