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Globally constrained forest biophysical cooling benefits under rising atmospheric dryness


Abstract

Climate change reshapes forest biophysical effects, yet the impact direction and strength remain uncertain. Here we quantify the growing-season land surface temperature between forests and adjacent open land (∆LSTgs) and show contrasting temporal trends in ∆LSTgs across the globe during 2001–2023. Rising vapour pressure deficit (VPD) has emerged as the primary driver of these contrasting trends, surpassing other common climatic factors. By contrast, plant anisohydricity—an indicator of stomatal regulation behaviour—is the most important forest trait that negatively modulates the strength of the ∆LSTgs response to VPD variability. At low latitudes, forests are more isohydric, and rising VPD has exceeded the hydraulic safety margin, resulting in weakened cooling. Conversely, high-latitude forests are more anisohydric; VPD remains below the safety margin, and rising VPD thus leads to enhanced cooling. These results highlight that the overall climate benefits of global forests may be undermined if global VPD continues to intensify in future.

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Fig. 1: Temporal changes in the biophysical effect of global forests on land surface temperatures (ΔLSTgs) under increasing VPD.
The alternative text for this image may have been generated using AI.
Fig. 2: Anisohydricity of forest ecosystems determines the strength of SΔLSTgs_VPD.
The alternative text for this image may have been generated using AI.
Fig. 3: Schematic diagram describing plant stomatal behaviour, energy fluxes and biophysical effects under varying VPD conditions in isohydric and anisohydric forests.
The alternative text for this image may have been generated using AI.
Fig. 4: The VPDsafetyfor maintaining a biophysical cooling in global forests.
The alternative text for this image may have been generated using AI.

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Amplified local cooling effect of forestation in warming Europe

Data availability

The global VOD, LST, NDVI, VPD, WS, SW, Pre, SM, Tmin, Tmax, Tmean, tree height, tree cover, tree age, AGB, forest types, tree richness, LAI, root depth, SN, SOC and SCC data used for the analyses in this study are available online as follows. LPRM AMSR-E VOD: https://disc.gsfc.nasa.gov/datasets/LPRM_AMSRE_A_SOILM3_002/summary, https://disc.gsfc.nasa.gov/datasets/LPRM_AMSRE_D_SOILM3_002/summary, https://disc.gsfc.nasa.gov/datasets/LPRM_AMSR2_A_SOILM3_001/summary, https://disc.gsfc.nasa.gov/datasets/LPRM_AMSR2_D_SOILM3_001/summary; IMERG Precipitation: https://gpm.nasa.gov/data/directory; MOD11C3 LST product: https://lpdaac.usgs.gov/products/mod11c3v061/; TerraClimate VPD, SW, PRE, SM, Tmin, Tmax, Tmean product: https://www.climatologylab.org/terraclimate.html; CO2 product https://db.cger.nies.go.jp/dataset/ODIAC/DL_odiac2024.html; tree height product: https://glad.umd.edu/dataset/gedi/; tree cover product: https://glad.earthengine.app/view/global-forest-change; MOD13C2 NDVI product: https://lpdaac.usgs.gov/products/mod13c2v061/; above-ground biomass product: https://climate.esa.int/en/projects/biomass/data/; MCD12C1 forest type product: https://lpdaac.usgs.gov/products/mcd12c1v061/; MCD15A2H LAI product: https://www.earthdata.nasa.gov/data/catalog/lpcloud-mcd15a2h-061; SoilGrids SN, SCC, SOC: https://files.isric.org/soilgrids/latest/; tree richness dataset: https://doi.org/10.6084/m9.figshare.20055488 (ref. 71); tree age dataset: https://essd.copernicus.org/articles/13/4881/2021/; root depth dataset: https://github.com/yalingliu-cu/plant-strategies; MCD43C3 albedo product: https://lpdaac.usgs.gov/products/mcd43c3v061/; MOD16A2 LE product: https://lpdaac.usgs.gov/products/mod16a2v061/. Other source data used for this analysis are available via Zenodo at https://doi.org/10.5281/zenodo.2017425 (ref. 84). Source data are provided with this paper.

Code availability

The code used for this analysis is available via Zenodo at https://doi.org/10.5281/zenodo.20174250 (ref. 84).

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Acknowledgements

This study was supported by the National Natural Science Foundation of China (grant nos. 42225104 and 42471326), the Science and Technology Program of Guangdong (grant no. 2024B1212070012), the General Program of Guangdong Provincial Natural Science Foundation (grant no. 2024A1515012731) and the Chinese Academy of Sciences Project for Young Scientists in Basic Research (grant no. YSBR-086)

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Y.S. designed the study and wrote the initial manuscript; C.Z. collected the data, performed the analyses and wrote the initial manuscript; Z.L., W.Z., P.C., S.J., Y.W., J.L., J.C., S.Z., Y.Z., A.C., J.M.C., J.S., R.L., J.W., X.F., K.Y., W.Y. and X.C. reviewed and edited the manuscript. All authors contributed to the interpretation of the results and approved the final version of the manuscript.

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Yongxian Su.

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Nature Climate Change thanks Jun Ge and the other, anonymous, reviewer(s) for their contribution to the peer review of this work.

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Supplementary Figs. 1–19 and References.

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Source Data Fig. 1 (download XLSX )

Statistical source data for Fig. 1, including temporal trends in ΔLSTgs and VPD during 2001–2023, RF-based climate-variable importance scores, dominant-predictor percentages, partial dependence data and piecewise regression fits for the ΔLSTgs–VPD relationship, spatial estimates of SΔLSTgs_VPD, and grid-by-grid comparisons of SΔLSTgs_VPD below and above VPDcrit.

Source Data Fig. 2 (download XLSX )

Statistical source data for Fig. 2, including ecosystem-trait importance estimates from linear regression, ridge regression, partial correlation analysis and sequential regression; moving-window correlations between ecosystem anisohydricity and SΔLSTgs_VPD; and ΔLSTgs–VPD response curves across ecosystem anisohydricity bins.

Source Data Fig. 4 (download XLSX )

Statistical source data for Fig. 4, including VPDsafety for sustaining the biophysical cooling effect of global forests, regional percentages of forests where VPD2023 exceeded or remained below VPDcrit, and regionally averaged VPDsafety values.

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Zhang, C., Su, Y., Liao, Z. et al. Globally constrained forest biophysical cooling benefits under rising atmospheric dryness.
Nat. Clim. Chang. (2026). https://doi.org/10.1038/s41558-026-02677-y

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