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A structural correction to atmospheric evaporative demand narrows the gap between offline aridity diagnostics and Earth system model projections
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  • Published: 05 January 2026

A structural correction to atmospheric evaporative demand narrows the gap between offline aridity diagnostics and Earth system model projections

  • Daeha Kim1 &
  • Minha Choi2,3 

npj Climate and Atmospheric Science , 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
  • Environmental sciences
  • Hydrology

Abstract

Offline aridity and drought diagnostics typically project widespread terrestrial drying under climate change, whereas fully coupled Earth system models (ESMs) often simulate modest or regionally heterogeneous changes—and in some regions increasing—runoff. This long-standing divergence has been attributed largely to missing vegetation physiological effects and the neglect of sub-annual climate variability in offline diagnostic frameworks. Here, we show that a more fundamental issue is the violation of the diagnostic framework’s structural requirement that potential evapotranspiration (PET) and precipitation (P) act as independent climatic constraints. Using Penman and Penman–Monteith formulations, each with and without thermodynamic deflation via the complementary evaporation principle (CEP), we demonstrate that land–atmosphere feedbacks embedded in conventional PET estimates induce strong negative P–PET correlations (−0.45 ± 0.29; mean ± standard deviation) across land surfaces, which collapse toward near zero (−0.02 ± 0.42) after CEP deflation. Preserving PET–P independence substantially reduces inflation of the aridity index and brings offline diagnostic ET trends closer to ESM projections under a strong-emission scenario (from +0.61 to +0.39 mm yr−2; ESM mean: +0.28 mm yr−2). These results indicate that structural inconsistencies—rather than missing physiological processes alone—play a central role in the mismatch between offline diagnostics and ESM hydrology. Ensuring that PET is not inflated by land–atmosphere feedbacks is therefore essential for theoretically valid offline hydrologic assessments under a warming climate.

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Data availability

The ERA5 reanalysis and CMIP6 datasets used to reproduce the results of this study are publicly available from the Copernicus Climate Data Store (https://cds.climate.copernicus.eu/) and the IPSL ESGF node (https://esgf-node.ipsl.upmc.fr/projects/cmip6-ipsl/), respectively. The downscaled [CO2] dataset is accessible at Zenodo (https://zenodo.org/records/5021361).

Code availability

Python scripts used to estimate PET from meteorological inputs and to apply the CEP deflation are available upon reasonable requests from the first author (daeha.kim@jbnu.ac.kr).

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Acknowledgements

This work was supported by the National Research Foundation of Korea (NRF) grant funded by the Korea government (MSIT) (RS-2024-00416443).

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Authors and Affiliations

  1. Department of Civil Engineering, Jeonbuk National University, Jeonju, Jeonbuk State, Republic of Korea

    Daeha Kim

  2. School of Civil, Architectural Engineering & Landscape Architecture, Sungkyunkwan University, Suwon, Republic of Korea

    Minha Choi

  3. Department of Global Smart City, Sungkyunkwan University, Suwon, Republic of Korea

    Minha Choi

Authors
  1. Daeha Kim
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  2. Minha Choi
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Contributions

D.K. conceived the study, performed the calculations, generated the visualizations, drafted the manuscript, and led the interpretation and discussion of the results. M.C. contributed to the discussion, interpretation, and revision of the manuscript. All authors reviewed and approved the final manuscript.

Corresponding author

Correspondence to Minha Choi.

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Kim, D., Choi, M. A structural correction to atmospheric evaporative demand narrows the gap between offline aridity diagnostics and Earth system model projections. npj Clim Atmos Sci (2026). https://doi.org/10.1038/s41612-025-01306-3

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  • Received: 13 August 2025

  • Accepted: 19 December 2025

  • Published: 05 January 2026

  • DOI: https://doi.org/10.1038/s41612-025-01306-3

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