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Increased occurrences of consecutive La Niña events under global warming

Author

Listed:
  • Tao Geng

    (Laoshan Laboratory
    Ocean University of China)

  • Fan Jia

    (Chinese Academy of Sciences, and Laoshan Laboratory)

  • Wenju Cai

    (Ocean University of China
    CSIRO Oceans and Atmosphere
    Chinese Academy of Sciences)

  • Lixin Wu

    (Laoshan Laboratory
    Ocean University of China)

  • Bolan Gan

    (Ocean University of China)

  • Zhao Jing

    (Laoshan Laboratory
    Ocean University of China)

  • Shujun Li

    (Ocean University of China)

  • Michael J. McPhaden

    (NOAA Pacific Marine Environmental Laboratory)

Abstract

Most El Niño events occur sporadically and peak in a single winter1–3, whereas La Niña tends to develop after an El Niño and last for two years or longer4–7. Relative to single-year La Niña, consecutive La Niña features meridionally broader easterly winds and hence a slower heat recharge of the equatorial Pacific6,7, enabling the cold anomalies to persist, exerting prolonged impacts on global climate, ecosystems and agriculture8–13. Future changes to multi-year-long La Niña events remain unknown. Here, using climate models under future greenhouse-gas forcings14, we find an increased frequency of consecutive La Niña ranging from 19 ± 11% in a low-emission scenario to 33 ± 13% in a high-emission scenario, supported by an inter-model consensus stronger in higher-emission scenarios. Under greenhouse warming, a mean-state warming maximum in the subtropical northeastern Pacific enhances the regional thermodynamic response to perturbations, generating anomalous easterlies that are further northward than in the twentieth century in response to El Niño warm anomalies. The sensitivity of the northward-broadened anomaly pattern is further increased by a warming maximum in the equatorial eastern Pacific. The slower heat recharge associated with the northward-broadened easterly anomalies facilitates the cold anomalies of the first-year La Niña to persist into a second-year La Niña. Thus, climate extremes as seen during historical consecutive La Niña episodes probably occur more frequently in the twenty-first century.

Suggested Citation

  • Tao Geng & Fan Jia & Wenju Cai & Lixin Wu & Bolan Gan & Zhao Jing & Shujun Li & Michael J. McPhaden, 2023. "Increased occurrences of consecutive La Niña events under global warming," Nature, Nature, vol. 619(7971), pages 774-781, July.
  • Handle: RePEc:nat:nature:v:619:y:2023:i:7971:d:10.1038_s41586-023-06236-9
    DOI: 10.1038/s41586-023-06236-9
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    Cited by:

    1. Hui Chen & Yishuai Jin & Zhengyu Liu & Daoxun Sun & Xianyao Chen & Michael J. McPhaden & Antonietta Capotondi & Xiaopei Lin, 2024. "Central-Pacific El Niño-Southern Oscillation less predictable under greenhouse warming," Nature Communications, Nature, vol. 15(1), pages 1-10, December.
    2. Chen, Yan & Zhang, Ruiqian & Lyu, Jiayi & Ma, Xin, 2024. "The butterfly effect of cloud computing on the low-carbon economy," Technological Forecasting and Social Change, Elsevier, vol. 204(C).

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