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Volcanic eruptions disrupt ENSO teleconnections with land summer temperature

Author

Listed:
  • Xu Zhang

    (The University of Hong Kong
    The University of Hong Kong
    HKU Shenzhen Institute of Research and Innovation)

  • Jinbao Li

    (The University of Hong Kong
    The University of Hong Kong
    HKU Shenzhen Institute of Research and Innovation)

  • Shang-Ping Xie

    (University of California San Diego)

  • Fei Liu

    (Sun Yat-Sen University)

  • Feng Shi

    (Chinese Academy of Sciences)

  • Cong Gao

    (The University of Hong Kong)

  • Han Zhang

    (The University of Hong Kong
    South China Normal University)

  • Qianjin Dong

    (Wuhan University)

Abstract

The El Niño–Southern Oscillation (ENSO) is a key ocean-atmospheric mode that affects global weather and climate through atmospheric teleconnections. It remains unclear how robust and stable ENSO teleconnection patterns are under external perturbations. Here, we use observations to demonstrate that volcanic eruptions disrupt ENSO teleconnections with land surface air temperature in boreal summer across the globe. During eruption years, correlations are found to shift in 62.27% of regions where temperature is significantly connected to ENSO during non-eruption years. State-of-the-art Earth System Models fail to capture this disruptive effect, highlighting challenges in simulating the patterns of climate anomalies and extremes under external perturbations. The disruptive effect identified here raises questions about the stationarity assumption in ENSO reconstructions based upon temperature-sensitive proxy records. Our findings call for an improved characterization of regional climate impacts following volcanic eruptions.

Suggested Citation

  • Xu Zhang & Jinbao Li & Shang-Ping Xie & Fei Liu & Feng Shi & Cong Gao & Han Zhang & Qianjin Dong, 2025. "Volcanic eruptions disrupt ENSO teleconnections with land summer temperature," Nature Communications, Nature, vol. 16(1), pages 1-11, December.
  • Handle: RePEc:nat:natcom:v:16:y:2025:i:1:d:10.1038_s41467-025-64879-w
    DOI: 10.1038/s41467-025-64879-w
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