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Large-scale circulation drives atmospheric river landfall in the western United States
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  • Published: 10 February 2026

Large-scale circulation drives atmospheric river landfall in the western United States

  • Chanil Park  ORCID: orcid.org/0000-0002-2563-25281,2 &
  • Yi Ming1,3 

Communications Earth & Environment , 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

  • Atmospheric dynamics
  • Hydrology

Abstract

Atmospheric rivers cause extreme precipitation and sustain water resources in the western United States. Their occurrence has often been attributed to extratropical cyclones. Here, we apply a recently proposed multiscale index to atmospheric rivers identified from reanalysis data and show that their landfalls in this region are not merely synoptic-scale phenomena but are also driven by large-scale circulation independent of extratropical cyclones. Specifically, quasi-stationary waves with centers of action along the Eurasian and North American coasts form a circum-North Pacific pattern. This large-scale teleconnection pattern channels subtropical moisture toward the U.S. West Coast on intraseasonal timescales, enabling its constructive interference with extratropical cyclone-induced moisture transport. The resulting “intermediate” atmospheric rivers account for up to twice as much winter precipitation as purely synoptic atmospheric rivers and exhibit a stronger correspondence with high-category events. Recognizing this multiscale process will be critical for the improved understanding of their predictability, variability and projected changes.

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Data availability

The ERA5 data are accessible at https://cds.climate.copernicus.eu/datasets/reanalysis-era5-pressure-levels?tab=overview. The CPC precipitation data can be downloaded from https://psl.noaa.gov/data/gridded/data.cpc.globalprecip.html. The Niño 3.4 index can be accessed at https://psl.noaa.gov/data/timeseries/month/DS/Nino34/. The authors-produced AR catalogs, labeled with MI, are available upon request from CP (parkcha@bc.edu, cpark15@alaska.edu). The ARTMIP AR catalogs are available from the Climate Data Gateway of the ARTMIP. The data used for producing figures are available at Zenodo (https://zenodo.org/records/18349404).

Code availability

All the codes used to produce the results of the present study are available upon request from CP (parkcha@bc.edu, cpark15@alaska.edu).

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Acknowledgements

This study was funded by the U.S. NOAA through Grant NA23OAR4310132. Chanil Park was also supported by Basic Science Research Program through the NRF of Korea funded by the Ministry of Education (RS-2024-00406720).

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Authors and Affiliations

  1. Department of Earth and Environmental Sciences, Boston College, Chestnut Hill, MA, US

    Chanil Park & Yi Ming

  2. International Arctic Research Center, University of Alaska Fairbanks, Fairbanks, AK, US

    Chanil Park

  3. Schiller Institute for Integrated Science and Society, Boston College, Chestnut Hill, MA, US

    Yi Ming

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  1. Chanil Park
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C.P. conceptualized the study and performed the initial analysis. The manuscript was written by C.P. and revised by Y.M. Both authors contributed to the interpretation and discussion of the results.

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Correspondence to Chanil Park.

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Supplementary Movie 1 | Temporal evolution of two landfalling AR types

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Park, C., Ming, Y. Large-scale circulation drives atmospheric river landfall in the western United States. Commun Earth Environ (2026). https://doi.org/10.1038/s43247-026-03281-w

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  • Received: 15 August 2025

  • Accepted: 29 January 2026

  • Published: 10 February 2026

  • DOI: https://doi.org/10.1038/s43247-026-03281-w

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