Abstract
Compound dry-hot extremes exert stronger environmental impacts than individual dry or hot extremes. While evidence for increasing meteorological compound dry-hot extremes (defined using surface air temperature and vapor pressure deficit or precipitation) is growing, the impacts and evolving risks of soil-based compound dry-hot extremes remain poorly understood. Using homogenized soil temperature observations and observationally constrained soil moisture dataset for China, we show that the adverse effects of soil-based compound dry-hot extremes on vegetation productivity are more severe than their meteorological counterparts. From 1980 to 2017, the frequency and coverage area of soil-based compound dry-hot extremes in China increased by 3.0 days and 141.9(times)104 km2, respectively, with the most pronounced increases occurring in northern China. These increases are primarily attributed to anthropogenic soil warming. Under a fossil-fueled development scenario, the mean frequency of such extremes is projected to increase by 13.3 days by the end of the twenty-first century relative to the 1981–2010 baseline, potentially reducing China’s terrestrial vegetation gross primary production by approximately 0.025 Pg C a−1. Our findings highlight an anthropogenic escalation of soil-based compound dry-hot extremes and their growing threats to terrestrial carbon sinks and food security.
Similar content being viewed by others
Synergistic effects of high atmospheric and soil dryness on record-breaking decreases in vegetation productivity over Southwest China in 2023
Interaction between dry and hot extremes at a global scale using a cascade modeling framework
Anthropogenic enhancement of subsurface soil moisture droughts
Data availability
All data supporting the findings are publicly available. The gridded daily soil temperature data are available at https://www.scidb.cn/en/detail?dataSetId=765528002485288960&version=V3. The GLEAM4 dataset (soil moisture, surface sensible and latent heat fluxes) is from https://www.gleam.eu/. The GPP, SIF, and NPP data can be downloaded from https://daac.ornl.gov/VEGETATION/guides/FluxSat_GPP_FPAR.html, https://doi.org/10.6084/m9.figshare.6387494, and https://acdisc.gsfc.nasa.gov/data/CMS/MICASA_FLUX_D.1, respectively. The CN05.1 data can be secured through https://ccrc.iap.ac.cn/resource/detail?id=228. The global daily SPEI dataset is available at https://doi.org/10.5281/zenodo.8060268. The ERA5 reanalysis data is available at https://www.ecmwf.int/en/forecasts/dataset/ecmwf-reanalysis-v5. The land-use/land-cover dataset is available at https://zenodo.org/records/4417810. The model simulation data can be downloaded from https://pcmdi.llnl.gov/CMIP6/. The raw data to reproduce the figures of the paper are available at https://doi.org/10.6084/m9.figshare.2841542068.
Code availability
The codes supporting this study are available at https://doi.org/10.6084/m9.figshare.2841542068.
References
Hao, Y. et al. Probabilistic assessments of the impacts of compound dry and hot events on global vegetation during growing seasons. Environ. Res. Lett. 16, 074055 (2021).
Zhao, H. et al. U.S. winter wheat yield loss attributed to compound hot-dry-windy events. Nat. Commun. 13, 7233 (2022).
Richardson, D. et al. Global increase in wildfire potential from compound fire weather and drought. npj Clim. Atmos. Sci. 5, 23 (2022).
Yin, J. et al. Future socio-ecosystem productivity threatened by compound drought–heatwave events. Nat. Sustain. 6, 259–272 (2023).
Yao, Y. et al. Compound hot-dry events greatly prolong the recovery time of dryland ecosystems. Natl. Sci. Rev. 11, nwae274 (2024).
Jiang, L. et al. Increased frequency and severity of global compound dry and heat wave events in a daily scale. J. Hydrol. 654, 132857 (2025).
Chen, D. et al. Contribution of anthropogenic influence to the 2022-like Yangtze River valley compound heatwave and drought event. npj Clim. Atmos. Sci. 7, 172 (2024).
Tripathy, K. P. & Mishra, A. K. How unusual is the 2022 European Compound Drought and Heatwave Event? Geophys. Res. Lett. 50, e2023GL105453 (2023).
Tripathy, K. P., Mukherjee, S., Mishra, A. K., Mann, M. E. & Williams, A. P. Climate change will accelerate the high-end risk of compound drought and heatwave events. Proc. Natl. Acad. Sci. USA 120, e2219825120 (2023).
Hao, Z. et al. Compound droughts and hot extremes: characteristics, drivers, changes, and impacts. Earth Sci. Rev. 235, 104241 (2022).
Seneviratne, S. I. et al. Investigating soil moisture-climate interactions in a changing climate: a review. Earth Sci. Rev. 99, 125–161 (2010).
Miralles, D. G., van den Berg, M. J., Teuling, A. J. & de Jeu, R. A. M. Soil moisture-temperature coupling: a multiscale observational analysis. Geophys. Res. Lett. 39, L21707 (2012).
Alizadeh, M. R. et al. A century of observations reveals increasing likelihood of continental-scale compound dry-hot extremes. Sci. Adv. 6, eaaz4571 (2020).
Zscheischler, J. & Seneviratne, S. I. Dependence of drivers affects risks associated with compound events. Sci. Adv. 3, e1700263 (2017).
Zeng, J. et al. Comparison of the risks and drivers of compound hot-dry and hot-wet extremes in a warming world. Environ. Res. Lett. 19, 114026 (2024).
Zhang, X. et al. Amplification of coupled hot-dry extremes over eastern monsoon China. Earth’s Future 11, e2023EF003604 (2023).
Fan, Y. et al. A critical review for real-time continuous soil monitoring: advantages, challenges, and perspectives. Environ. Sci. Technol. 56, 13546–13564 (2022).
Pastorello, G. et al. The FLUXNET2015 dataset and the ONEFlux processing pipeline for eddy covariance data. Sci. Data 7, 225 (2020).
Jiang, M. et al. Seamless global daily soil moisture mapping using deep learning based spatiotemporal fusion. Int. J. Appl. Earth Obs. 139, 104517 (2025).
Pokhrel, Y. et al. Global terrestrial water storage and drought severity under climate change. Nat. Clim. Change 11, 226–233 (2021).
Hosseinzadehtalaei, P., Termonia, P. & Tabari, H. Projected changes in compound hot-dry events depend on the dry indicator considered. Commun. Earth Environ. 5, 220 (2024).
García-García, A. et al. Soil heat extremes can outpace air temperature extremes. Nat. Clim. Change 13, 1237–1241 (2023).
Liu, L. et al. Soil moisture dominates dryness stress on ecosystem production globally. Nat. Commun. 11, 4892 (2020).
Li, W. et al. Widespread increasing vegetation sensitivity to soil moisture. Nat. Commun. 13, 3959 (2022).
Sharma, P. K. & Kumar, S. Soil temperature and plant growth. Springer, Cham. 175–204 (2023).
Liu, Y. et al. Soil temperature dominates forest spring phenology in China. Agric. Meteorol. 355, 110141 (2024).
Wang, C. et al. The temperature sensitivity of soil: microbial biodiversity, growth, and carbon mineralization. ISME J. 15, 2738–2747 (2021).
Hursh, A. et al. The sensitivity of soil respiration to soil temperature, moisture, and carbon supply at the global scale. Glob. Change Biol. 23, 2090–2103 (2017).
Yuan, D. et al. Species-specific indication of 13 tree species growth on climate warming in temperate forest community of northeast China. Ecol. Indic. 133, 108389 (2021).
Ridder, N. N. et al. Global hotspots for the occurrence of compound events. Nat. Commun. 11, 5956 (2020).
Vicente-Serrano, S. M., Beguería, S. & López-Moreno, J. I. A. Multi-scalar drought index sensitive to global warming: the Standardized Precipitation Evapotranspiration Index. J. Clim. 23, 1696–1718 (2010).
Törnros, T. & Menzel, L. Addressing drought conditions under current and future climates in the Jordan River region. Hydrol. Earth Syst. Sci. 18, 305–318 (2014).
Wang, H., Rogers, J. C. & Munroe, D. K. Commonly used drought indices as indicators of soil moisture in China. J. Hydrometeor. 16, 1397–1408 (2015).
Gevaert, A. I., Miralles, D. G., de Jeu, R. A. M., Schellekens, J. & Dolman, A. J. Soil moisture-temperature coupling in a set of land surface models. J. Geophys. Res. Atmos. 123, 1481–1498 (2018).
Yuan, Q. et al. Coupling of soil moisture and air temperature from multiyear data during 1980–2013 over China. Atmosphere 11, 25 (2020).
Abu-Hamdeh, N. H. Thermal properties of soils as affected by density and water content. Biosyst. Eng. 86, 97–102 (2003).
Al-Kayssi, A. W., Al-Karaghouli, A. A., Hasson, A. M. & Beker, S. A. Influence of soil moisture content on soil temperature and heat storage under greenhouse conditions. J. Agric. Eng. Res. 45, 241–252 (1990).
Gillett, N. P. et al. The Detection and Attribution Model Intercomparison Project (DAMIP v1.0) contribution to CMIP6. Geosci. Model Dev. 9, 3685–3697 (2016).
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).
Bevacqua, E. et al. Precipitation trends determine future occurrences of compound hot–dry events. Nat. Clim. Chang. 12, 350–355 (2022).
Hong, H., Sun, J. & Wang, H. Interdecadal variation in the frequency of extreme hot events in Northeast China and the possible mechanism. Atmos. Res. 244, 105065 (2020).
Meinshausen, M. et al. The shared socio-economic pathway (SSP) greenhouse gas concentrations and their extensions to 2500. Geosci. Model Dev. 13, 3571–3605 (2020).
Jansson, J. K. & Hofmockel, K. S. Soil microbiomes and climate change. Nat. Rev. Microbiol. 18, 35–46 (2020).
Robinson, S. I., McLaughlin, ÓB., Marteinsdóttir, B. & O’Gorman, E. J. Soil temperature effects on the structure and diversity of plant and invertebrate communities in a natural warming experiment. J. Anim. Ecol. 87, 634–646 (2018).
Bossio, D. A. et al. The role of soil carbon in natural climate solutions. Nat. Sustain. 3, 391–398 (2020).
Delgado-Baquerizo, M. et al. The proportion of soil-borne pathogens increases with warming at the global scale. Nat. Clim. Chang. 10, 550–554 (2020).
Neußner, O. Early warning alerts for extreme natural hazard events: a review of worldwide practices. Int. J. Disaster Risk Reduct. 60, 102295 (2021).
Ghanbari, M. et al. The role of climate change and urban development on compound dry-hot extremes across US cities. Nat. Commun. 14, 3509 (2023).
Liu, Y., Chen, X., Bai, Y. & Zeng, J. Evaluation of 22 CMIP6 model-derived global soil moisture products of different shared socioeconomic pathways. J. Hydrol. 636, 131241 (2024).
Zhou, J., Zhang, J. & Huang, Y. Evaluation of soil temperature in CMIP6 multimodel simulations. Agric. Meteorol. 352, 110039 (2024).
Wang, D., Wang, A. & Kong, X. Homogenization of the daily land surface temperature over the mainland of China from 1960 through 2017. Adv. Atmos. Sci. 38, 1811–1822 (2021).
Szentimrey, T. Overview of mathematical background of homogenization, summary of method MASH and comments on benchmark validation. Int. J. Climatol. 43, 6314–6329 (2023).
Miralles, D. G. et al. GLEAM4: global land evaporation and soil moisture dataset at 0.1°resolution from 1980 to near present. Sci. Data 12, 416 (2025).
Wu, J. & Gao, X. A gridded daily observation dataset over China region and comparison with the other datasets. Chin. J. Geophys. 56, 1102–1111 (2013).
Yuan, W. et al. Increased atmospheric vapor pressure deficit reduces global vegetation growth. Sci. Adv. 5, eaax1396 (2019).
Liu, X. et al. The first global multi-timescale daily SPEI dataset from 1982 to 2021. Sci. Data 11, 223 (2024).
Joiner, J. et al. Estimation of terrestrial global Gross Primary Production (GPP) with satellite data-driven models and eddy covariance flux data. Remote Sens. 10, 1346 (2018).
Zhang, Y., Joiner, J., Alemohammad, S. H., Zhou, S. & Gentine, P. A global spatially contiguous solar-induced fluorescence (CSIF) dataset using neural networks. Biogeosciences 15, 5779–5800 (2018).
Randerson, J. T., Thompson, M. V., Malmstrom, C. M., Field, C. B. & Fung, I. Y. Substrate limitations for heterotrophs: implications for models that estimate the seasonal cycle of atmospheric CO2. Glob. Biogeochem. Cycles 10, 585–602 (1996).
Hersbach, H. et al. The ERA5 global reanalysis. Q. J. Roy. Meteorol. Soc. 146, 1999–2049 (2020).
Yang, J. & Huang, X. The 30 m annual land cover dataset and its dynamics in China from 1990 to 2019. Earth Syst. Sci. Data 13, 3907–3925 (2021).
Olonscheck, D. et al. The new Max Planck Institute Grand Ensemble with CMIP6 forcing and high-frequency model output. J. Adv. Model Earth. Syst. 15, e2023MS003790 (2023).
Keeling, C. D. et al. Atmospheric carbon dioxide variations at Mauna Loa Observatory, Hawaii. Tellus 28, 538–551 (1976).
Sen, P. K. Estimates of the regression coefficient based on Kendall’s tau. J. Am. Stat. Assoc. 63, 1379–1389 (1968).
Mann, H. B. Nonparametric tests against trend. Econometrica 13, 245–259 (1945).
Kendall, M. G. Rank Correlation Methods (Griffin, 1975).
Hollander, M. & Wolfe, D. Nonparametric Statistical Methods Ch 9, 207–208 (John Wiley & Sons, 1973).
Liang, et al. Anthropogenically-driven escalating impact of soil-based compound dry-hot extremes on vegetation productivity. figshare. Dataset. https://doi.org/10.6084/m9.figshare.28415420 (2025).
Acknowledgements
Our sincere gratitude goes to the researchers and institutions responsible for the development, compilation, and public release of the datasets employed in this study. Their efforts in advancing open data sharing have laid a critical foundation for this work. This work was supported by the National Natural Science Foundation of China (42522102, 42275040) and the Programme of Kezhen-Bingwei Excellent Young Scientists of the Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences (2022RC006).
Author information
Authors and Affiliations
Contributions
J.W. and Q.G. conceived and designed the study. Y.L. and J.W. performed the analyses. J.W. and Y.L. wrote the draft. J.W., Q.G., Z.H., H.W., and H.C. reviewed, revised, and edited the manuscript. All authors contributed to interpreting the results.
Corresponding authors
Ethics declarations
Competing interests
The authors declare no competing interests.
Peer review
Peer review information
Nature Communications thanks Wanjuan Song, Duminda Vidana and the other anonymous, reviewer(s) for their contribution to the peer review of this work. A peer review file is available.
Additional information
Publisher’s note Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.
Supplementary information
Supplementary Information
Peer Review File
Reporting Summary
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/.
Reprints and permissions
About this article
Cite this article
Liang, Y., Wang, J., Hao, Z. et al. Anthropogenically-driven escalating impact of soil-based compound dry-hot extremes on vegetation productivity.
Nat Commun (2026). https://doi.org/10.1038/s41467-026-68878-3
Received:
Accepted:
Published:
DOI: https://doi.org/10.1038/s41467-026-68878-3
Source: Ecology - nature.com
