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Ocean dynamics shape marine heatwaves and their predictability
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  • Published: 18 February 2026

Ocean dynamics shape marine heatwaves and their predictability

  • Xianglin Ren1,
  • Wei Liu  ORCID: orcid.org/0000-0001-5958-37391 &
  • Liping Zhang  ORCID: orcid.org/0000-0003-1122-89272,3 

Nature Communications , Article number:  (2026) Cite this article

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We are providing an unedited version of this manuscript to give early access to its findings. Before final publication, the manuscript will undergo further editing. Please note there may be errors present which affect the content, and all legal disclaimers apply.

Subjects

  • Climate sciences
  • Ocean sciences

Abstract

Marine heatwaves have become more frequent and intense under anthropogenic warming, posing increasing threats to marine ecosystems and coastal societies, necessitating a better understanding of their mechanism and predictability. Here we show how ocean dynamics modulate marine heatwaves globally by comparing dynamic and slab ocean climate model simulations. We discover that ocean dynamics significantly promote marine heatwave intensity and duration in mid-to-high latitude oceans, as well as the eastern tropical Pacific where marine heatwaves are inherently linked to extreme El Niño events. Our mixed-layer heat budget analysis unravels that heat accumulation during marine heatwave episodes is strongly influenced by vertical mixing and horizontal transport processes, so that warm sea surface temperature extremes in dynamic ocean differ in magnitude and evolution rhythm from those in slab ocean. We further find robust multi-year potential predictability of marine heatwave in the North Atlantic with a dynamic ocean, owing primarily to the predictability of the Atlantic Meridional Overturning Circulation. Our findings emphasize the irreplaceable role of oceanic dynamics in marine heatwave evolution and predictability, with important implications for future climate extreme prediction and adaptation strategies.

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Data availability

CESM1 model data are available at https://gdex.ucar.edu/datasets/d651027/dataaccess/. CMIP3 model data are available at https://aims2.llnl.gov/search. ERSSTv5 data are available at https://www.ncei.noaa.gov/products/extended-reconstructed-sst. CMAP Precipitation data are available at https://psl.noaa.gov/data/gridded/data.cmap.html.

Code availability

Figures are generated via the NCAR Command Language (NCL, Version 6.5.0) [Software]. (2018). Boulder, Colorado: UCAR/NCAR/CISL/TDD (https://doi.org/10.5065/D6WD3XH5). The codes to generate Figs. 1–5 are available from Zenodo66 at https://doi.org/10.5281/zenodo.18357158.

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Acknowledgements

This study has been supported by U.S. National Science Foundation (OCE-2123422, AGS-2053121, and AGS-2237743). We thank Timothy M. DelSole for helpful comments and suggestions.

Author information

Authors and Affiliations

  1. Department of Earth Sciences and Planetary Sciences, University of California Riverside, Riverside, CA, USA

    Xianglin Ren & Wei Liu

  2. NOAA/Geophysical Fluid Dynamics Laboratory, Princeton, NJ, USA

    Liping Zhang

  3. University Corporation for Atmospheric Research, Boulder, CO, USA

    Liping Zhang

Authors
  1. Xianglin Ren
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  2. Wei Liu
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Contributions

X.R. performed the analysis and wrote the original draft of the paper. W.L. conceived the study. L.Z. guided the predictability analysis. All authors contributed to interpreting the results and made improvements to the paper.

Corresponding author

Correspondence to Wei Liu.

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Ren, X., Liu, W. & Zhang, L. Ocean dynamics shape marine heatwaves and their predictability. Nat Commun (2026). https://doi.org/10.1038/s41467-026-69509-7

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  • Received: 20 August 2025

  • Accepted: 03 February 2026

  • Published: 18 February 2026

  • DOI: https://doi.org/10.1038/s41467-026-69509-7

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