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.
Similar content being viewed by others
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).
References
Vicente-Serrano, S. M. et al. Atmospheric drought indices in future projections. Nat. Water 3, 374–387 (2025).
Scheff, J., Coats, S. & Laguë, M. M. Why do the global warming responses of land-surface models and climatic dryness metrics disagree? Earths Future 10, e2022EF002814 (2022).
Yang, Y. et al. Hydrologic implications of vegetation response to elevated CO2 in climate projections. Nat. Clim. Change 9, 44–48 (2019).
Milly, P. C. & Dunne, K. A. Potential evapotranspiration and continental drying. Nat. Clim. Change 6, 946–949 (2016).
Yang, Y. et al. Comparing Palmer Drought Severity Index drought assessments using the traditional offline approach with direct climate model outputs. Hydrol. Earth Syst. Sci. 24, 2921–2930 (2020).
Kim, D., Chun, J. A., Yeo, J. H. & Ha, K. J. Divergent flash-drought risks indicated by evaporative stress and soil-moisture projections under warming scenarios. Environ. Res. Lett. 18, 094023 (2023).
Greve, P., Roderick, M. L., Ukkola, A. M. & Wada, Y. The aridity index under global warming. Environ. Res. Lett. 14, 124006 (2019).
Scheff, J. A unified wetting and drying theory. Nat. Clim. Change 9, 9–10 (2019).
Berg, A. & Sheffield, J. Climate change and drought: the soil-moisture perspective. Curr. Clim. Change Rep. 4, 180–191 (2018).
Milly, P. C. D. & Dunne, K. A. A hydrologic drying bias in water-resource impact analyses of anthropogenic climate change. J. Am. Water Resour. Assoc. 53, 822–838 (2017).
Roderick, M. L., Greve, P. & Farquhar, G. D. On the assessment of aridity with changes in atmospheric CO. Water Resour. Res. 51, 5450–5463 (2015).
Swann, A. L., Hoffman, F. M., Koven, C. D. & Randerson, J. T. Plant responses to increasing CO2 reduce estimates of climate impacts on drought severity. Proc. Natl Acad. Sci. USA 113, 10019–10024 (2016).
Lemordant, L. et al. Critical impact of vegetation physiology on the continental hydrologic cycle in response to increasing CO2. Proc. Natl Acad. Sci. USA 115, 4093–4098 (2018).
Scheff, J. Drought indices, drought impacts, CO2, and warming: a historical and geologic perspective. Curr. Clim. Change Rep. 4, 202–209 (2018).
Liu, Z. et al. A physically based potential evapotranspiration model for global water-availability projections. J. Hydrol. 622, 129767 (2023).
Lesk, C. S., Winter, J. M. & Mankin, J. S. Projected runoff declines from plant physiological effects on precipitation. Nat. Water 3, 167–177 (2025).
Scheff, J., Mankin, J. S., Coats, S. & Liu, H. CO2-plant effects do not account for the gap between dryness indices and projected dryness impacts in CMIP6 or CMIP5. Environ. Res. Lett. 16, 034018 (2021).
Mianabadi, A., Davary, K., Pourreza-Bilondi, M. & Coenders-Gerrits, A. M. J. Budyko framework: towards non-steady-state conditions. J. Hydrol. 588, 125089 (2020).
Roderick, M. L. & Farquhar, G. D. A simple framework for relating variations in runoff to variations in climatic conditions and catchment properties. Water Resour. Res. 47, W00G07 (2011).
Yang, H., Yang, D., Lei, Z. & Sun, F. New analytical derivation of the mean annual water-energy balance equation. Water Resour. Res. 44, W03410 (2008).
Crago, R. D. & Qualls, R. J. A graphical interpretation of the rescaled complementary relationship for evapotranspiration. Water Resour. Res. 57, e2020WR028299 (2021).
Szilagyi, J. On the thermodynamic foundations of the complementary relationship of evaporation. J. Hydrol. 593, 125916 (2021).
Han, S. & Tian, F. A review of the complementary principle of evaporation: from the original linear relationship to generalized nonlinear functions. Hydrol. Earth Syst. Sci. 24, 2269–2285 (2020).
Kim, D. & Chun, J. A. Revisiting a two-parameter Budyko equation with the complementary-evaporation principle for proper consideration of surface-energy balance. Water Resour. Res. 57, e2021WR030838 (2021).
Zhang, L. & Brutsaert, W. Blending the evaporation precipitation ratio with the complementary principle function for the prediction of evaporation. Water Resour. Res. 57, e2021WR029729 (2020).
Penman, H. L. Natural evaporation from open water, bare soil and grass. Proc. R. Soc. Lond. A 193, 120–145 (1948).
Lhomme, J. P. Towards a rational definition of potential evaporation. Hydrol. Earth Syst. Sci. 1, 257–264 (1997).
Penman, H. L. Evaporation: an introductory survey. Neth. J. Agric. Sci. 4, 9–29 (1956).
Monteith, J. L. Evaporation and environment. Symp. Soc. Exp. Biol. 19, 205–234 (1965).
Medlyn, B. E. et al. Reconciling the optimal and empirical approaches to modelling stomatal conductance. Glob. Change Biol. 17, 2134–2144 (2011).
Kim, D., Choi, M. & Kang, M. Testing new potential-evaporation formulations for identifying soil-moisture deficiency in agricultural areas under global warming. J. Hydrol. 661, 133760 (2025).
Soci, C. et al. The ERA5 global reanalysis from 1940 to 2022. Q. J. R. Meteorol. Soc. 150, 4014–4048 (2024).
Gebrechorkos, S. H. et al. Warming accelerates global drought severity. Nature 642, 628–635 (2025).
Zhou, S. et al. Land–atmosphere feedbacks exacerbate concurrent soil drought and atmospheric aridity. Proc. Natl Acad. Sci. USA 116, 18848–18853 (2019).
Szilagyi, J. Temperature corrections in the Priestley–Taylor equation of evaporation. J. Hydrol. 519, 455–464 (2014).
Huntington, J. L., Szilagyi, J., Tyler, S. W. & Pohll, G. M. Evaluating the complementary relationship for estimating evapotranspiration from arid shrublands. Water Resour. Res. 47, W05533 (2011).
Lobell, D. B. & Bonfils, C. The effect of irrigation on regional temperatures: a spatial and temporal analysis of trends in California, 1934–2002. J. Clim. 21, 2063–2071 (2008).
Szilagyi, J. & Schepers, A. Coupled heat and vapor transport: the thermostat effect of a freely evaporating land surface. Geophy. Res. Lett. 41, 435–441 (2014).
Seneviratne, S. I. et al. Investigating soil-moisture–climate interactions in a changing climate: a review. Earth-Sci. Rev. 99, 125–161 (2010).
Berg, A. et al. Land–atmosphere feedbacks amplify aridity increase over land under global warming. Nat. Clim. Change 6, 869–874 (2016).
Denissen, J. M. et al. Widespread shift from ecosystem energy to water limitation with climate change. Nat. Clim. Change 12, 677–684 (2022).
Andréassian, V. & Sari, T. On the puzzling similarity of two water-balance formulas—Turc–Mezentsev vs. Tixeront–Fu. Hydrol. Earth Syst. Sci. 23, 2339–2350 (2019).
Kidron, G. J. Comparing overland-flow processes between semiarid and humid regions: does saturation overland flow take place in semiarid regions? J. Hydrol. 593, 125624 (2021).
Eyring, V. et al. Overview of the Coupled Model Intercomparison Project Phase 6 (CMIP6) experimental design and organization. Geosci. Model Dev. 9, 1937–1958 (2016).
O’Neill, B. C. et al. The Scenario Model Intercomparison Project (ScenarioMIP) for CMIP6. Geosci. Model Dev. 9, 3461–3482 (2016).
Vicente-Serrano, S. M. et al. The uncertain role of rising atmospheric CO2 on global plant transpiration. Earth-Sci. Rev. 230, 104055 (2022).
Zaitchik, B. F., Rodell, M., Biasutti, M. & Seneviratne, S. I. Wetting and drying trends under climate change. Nat. Water 1, 502–513 (2023).
Zhou, S. & Yu, B. Neglecting land-atmosphere feedbacks overestimates climate-driven increases in evapotranspiration. Nat. Clim. Change 15, 1099–1106 (2025).
Lesk, C. et al. Stronger temperature–moisture couplings exacerbate the impact of climate warming on global crop yields. Nat. Food 2, 683–691 (2021).
Douville, H. et al. Drivers of the enhanced decline of land near-surface relative humidity to abrupt 4×CO2 in CNRM-CM6-1. Clim. Dyn. 55, 1613–1629 (2020).
Byrne, M. P. & O’Gorman, P. A. Understanding decreases in land relative humidity with global warming: conceptual model and GCM simulations. J. Clim. 29, 9045–9061 (2016).
Huang, J., Yu, H., Guan, X., Wang, G. & Guo, R. Accelerated dryland expansion under climate change. Nat. Clim. Change 6, 166–171 (2016).
Cheng, W. et al. Global monthly gridded atmospheric carbon-dioxide concentrations under historical and future scenarios. Sci. Data 9, 83 (2022).
Zhang, L., Hu, Z., Fan, J., Zhou, D. & Tang, F. A meta-analysis of the canopy light extinction coefficient in terrestrial ecosystems. Fron. Earth Sci. 8, 599–609 (2014).
Yang, K. et al. Turbulent flux transfer over bare-soil surfaces: characteristics and parameterization. J. Appl. Meteorol. Climatol. 47, 276–290 (2008).
Allen, R.G., Pereira, L.S., Raes, D. & Smith, M. Crop Evapotranspiration (guidelines for computing crop water requirements). FAO Irrigation and drainage paper No. 56. Food and Agriculture Organization of the United Nations, Rome, Italy (1998).
Lin, Y. S. et al. Optimal stomatal behaviour around the world. Nat. Clim. Change 5, 459–464 (2015).
Brutsaert, W. & Stricker, H. An advection-aridity approach to estimate actual regional evapotranspiration. Water Resour. Res. 15, 443–450 (1979).
Priestley, C. H. B. & Taylor, R. J. On the assessment of surface heat flux and evaporation using large-scale parameters. Mon. Weather Rev. 100, 81–92 (1972).
Szilagyi, J. & Crago, R. D. A thermodynamics-based versatile evapotranspiration-estimation method of minimum data requirement for water-resources investigations. J. Hydrol. 624, 129917 (2023).
Acknowledgements
This work was supported by the National Research Foundation of Korea (NRF) grant funded by the Korea government (MSIT) (RS-2024-00416443).
Author information
Authors and Affiliations
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
Ethics declarations
Competing interests
The authors declare no competing interests.
Additional information
Publisher’s note Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.
Supplementary information
Rights and permissions
Open Access This article is licensed under a Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License, which permits any non-commercial use, sharing, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if you modified the licensed material. You do not have permission under this licence to share adapted material derived from this article or parts of it. The images or other third party material in this article are included in the article’s Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by-nc-nd/4.0/.
About this article
Cite this article
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
Received:
Accepted:
Published:
DOI: https://doi.org/10.1038/s41612-025-01306-3


