Global climate mode resonance due to rapidly intensifying El Niño-Southern Oscillation

The El Niño-Southern Oscillation (ENSO) influences climate variability globally, encompassing various other modes of variability, and thus represents a key predictable climate signal on seasonal timescales. Yet, its response to greenhouse warming remains uncertain, with models projecting a range of outcomes. Here, we demonstrate that in response to warming, a state-of-the-art high-resolution climate model simulates a rapid transition from a moderate-amplitude irregular regime, as observed in the current climate, to a highly regular oscillation with intensifying amplitude. This behaviour can be attributed to increasing air-sea feedbacks, which approach criticality in the second half of this century, and growing atmospheric noise. As ENSO intensifies in this model, it synchronizes with other prominent climate modes, such as the North Atlantic Oscillation and the Indian Ocean Dipole, thereby imprinting its regular, predictable variability on them. If realized, this global climate mode resonance would have wide-ranging whiplash impacts on regional hydroclimates.

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Publication Details

Journal
Nature Communications
Published
2025-10-16
DOI
https://doi.org/10.1038/s41467-025-64619-0
Citations
4
Primary Topic
Climate variability and models
Type
article
Field-Weighted Citation Impact
4.42

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article

Global climate mode resonance due to rapidly intensifying El Niño-Southern Oscillation

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Nature Communications
Climate variability and models
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Global climate mode resonance due to rapidly intensifying El Niño-Southern Oscillation

Sun‐Seon Lee, Malte F. Stuecker, Axel Timmermann, Thomas Josef Jung, Ja-Yeon Moon, Sen Zhao, Tido Semmler, Rohit Ghosh, Fei‐Fei Jin
article en
4 citations

Abstract

The El Niño-Southern Oscillation (ENSO) influences climate variability globally, encompassing various other modes of variability, and thus represents a key predictable climate signal on seasonal timescales. Yet, its response to greenhouse warming remains uncertain, with models projecting a range of outcomes. Here, we demonstrate that in response to warming, a state-of-the-art high-resolution climate model simulates a rapid transition from a moderate-amplitude irregular regime, as observed in the current climate, to a highly regular oscillation with intensifying amplitude. This behaviour can be attributed to increasing air-sea feedbacks, which approach criticality in the second half of this century, and growing atmospheric noise. As ENSO intensifies in this model, it synchronizes with other prominent climate modes, such as the North Atlantic Oscillation and the Indian Ocean Dipole, thereby imprinting its regular, predictable variability on them. If realized, this global climate mode resonance would have wide-ranging whiplash impacts on regional hydroclimates.

Nature CommunicationsVol. 16(1)
University of Hawaiʻi at Mānoa (US), Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung (DE), University of Hawaii System (US), University of Bremen (DE), Pacific International Center for High Technology Research (US), Met Éireann (IE), Institute for Basic Science (KR), Pusan National University (KR), Pacific Biosciences (United States) (US)
National Science Foundation, U.S. Department of Energy, European Commission, Institute for Basic Science, European Climate, Infrastructure and Environment Executive Agency, Korea Research Environment Open Network, National Oceanic and Atmospheric Administration, Office of Science, Biological and Environmental Research, Climate Program Office
Openalex Percentile: Top 5%
Climate variability and models
4.42
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