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Crop water origins and hydroclimate vulnerability of global croplands

Abstract

Water availability critically influences crop phenology and agricultural productivity. Here we use satellite-derived water isotope observations and physical models to trace atmospheric moisture origins for major global rain-fed crops from 2003 to 2019, distinguishing between oceanic and terrestrial sources. Our analysis shows that the fraction of rainwater originating from land (f) varies both geographically and seasonally, with an important threshold at ~36%. Regions with higher f, that is, more dependent on land-originating water, are more prone to insufficient rainwater supply and soil moisture deficits during the main growing season. Crops in these regions show higher sensitivity to hydroclimate—with reduced productivity in lower-rainfall years—and a higher likelihood of drought. Notably, more than 40% of global maize and 60% of winter wheat is grown in regions where rainfall depends heavily on land-originating moisture (f ≥ 36%), underscoring the vulnerability of key staple crops to hydroclimate stress. Our results highlight the importance of managing local land moisture sources and reveal where targeted water management strategies would be most expected to enhance agricultural resilience.

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Fig. 1: Spatial and vertical patterns of δD and q during 2003–2019 from AIRS observations.
Fig. 2: Spatial patterns and annual cycle of the fraction of land-based moisture during 2003–2019 from AIRS observations.
Fig. 3: Sub-seasonal water dynamics encoded by atmospheric moisture sources f.
Fig. 4: f as an indicator for crop hydrological sensitivity.
Fig. 5: f as an indicator for crops sensitivity to droughts.

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Data availability

The cropland maps are available at https://glad.umd.edu/dataset/croplands. Crop calendar datasets are available at https://sage.nelson.wisc.edu/data-and-models/datasets/crop-calendar-dataset/. The TES products are available at https://asdc.larc.nasa.gov/project/TES/TL2HDOLN_6. The AIRS products are available via GES DISC at https://disc.gsfc.nasa.gov/datasets?keywords=tropess%20%2B%20airs%20%2B%20reanalysis&page=1 and EarthData at https://www.earthdata.nasa.gov/data/catalog?keyword=TROPESS%20AIRS-Aqua%20Reanalysis. The NIRv data calculated from the MCD43A4 are available at https://developers.google.com/earth-engine/datasets/catalog/MODIS_061_MCD43A4. The CSIF product is available via figshare at https://doi.org/10.6084/m9.figshare.6387494.v2 (ref. 76). The GLEAM datasets can be obtained from https://www.gleam.eu/. The ESI record is available at https://gee-community-catalog.org/projects/global_esi/?h=esi. Processed data are available via Zenodo at https://doi.org/10.5281/zenodo.15041289 (ref. 77).

Code availability

All analyses were conducted in Python (version 3.9,12); code is available via Github at https://github.com/yjiangc/water_isotope.

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Acknowledgements

This study was supported by the US National Science Foundation (NSF INFEWS #1639318) and the Center for Global Transformation at UC San Diego’s School of Global Policy and Strategy.

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Y.J. and J.A.B. designed the research. Y.J. analysed the data. Both authors wrote and revised the paper.

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Correspondence to Yan Jiang.

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Nature Sustainability thanks Xu Lian and the other, anonymous, reviewer(s) for their contribution to the peer review of this work.

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Extended data

Extended Data Fig. 1 Multiple year (2003-2019) mean annual vertical profiles of δD (‰).

Multiple year (2003-2019) mean annual vertical profiles of \({\boldsymbol{\delta }}{\boldsymbol{D}}\) (‰) over a, Eurasia, c, Asia, e, East Africa, g, Australia estimated from the AIRS. Multiple year mean \({\boldsymbol{q}}\) (g/kg) over b, Eurasia, d, Asia, f, East Africa, h, Australia. These complement Fig. 1 in the main manuscript to show the remaining regions of study not presented there.

Extended Data Fig. 2 Multiple year (2003-2019) mean seasonal cycle of precipitation (P, mm/day) and terrestrial moisture-contributed precipitation (P*f).

Multiple year (2003-2019) mean seasonal cycle of precipitation (P, mm/day) and terrestrial moisture-contributed precipitation (P*f) over a, North America, b, Eurasia, c, India, d, Asia, e, South America, f, Sahel, g, Southeastern Africa and h, Australia. Blue dots mark the peak rainfall amount. Shaded yellow areas present the general local growing season, where solid black lines are the start of the growing season and dashed black lines are the end of the growing season.

Extended Data Fig. 3 Multiple year (2003-2019) mean seasonal cycle of precipitation (P), potential evapotranspiration (PET), and RZSM anomaly.

Multiple year (2003-2019) mean seasonal cycle of precipitation (P), potential evapotranspiration (PET), and RZSM anomaly over a, North America, b, Eurasia, c, India, d, Asia, e, South America, f, Sahel, g, Southeastern Africa and h, Australia. Shades of each curve present the standard error of each observation. Shaded yellow areas present the general local growing season, where solid black lines are the start of the growing season and dashed black lines are the end of the growing season. The growing season is particularly long in Australia, for wheat is the main crop grown here (sowing starting in autumn and winter, harvesting occurring in spring and summer).

Extended Data Fig. 4 Subseasonal water dynamics indicated by the aridity index (AI).

a, Multiple-year mean seasonal cycles of precipitation (mm/day) and PET (mm/day) for the two groups seperated by the 0.65 AI threshold. b, The same as a, but for RZSM anomaly. Shaded areas present the standard error of each variable. c, Mean annual cycles of rainwater supply aggregated at different AI indices. d, The same as c, but for RZSM anomaly. The two solid lines indicate the general start and end of the merged crop growing season. The dashed line presents the general start of the harvest stage.

Extended Data Fig. 5 f as an indicator for different crops’ hydrological sensitivity.

a, Distribution of R2 of statistical model relating the maximum crop greenness (NIRvmax, a proxy for yield) to growing season hydrological parameters (rainwater supply and RZSM anomaly) for different major crops (Eq. 7). b, Mean R2 aggregated by different f values at 12% intervales for different crops. Shaded areas present the 25th and the 75th percentiles of R2.

Extended Data Fig. 6 Spatial patterns of R2 of the multiple linear regression model.

Spatial patterns of R2 of the multiple linear regression model for a, Maize. b, Rice. c, Soybean. d, Winter wheat. Grids marked with light orange are crop grids not included in the analysis. Girds marked with dots indicate statistical significance of the multiple linear regression model at the 90% confidence level and at least 90% accuracy using cross validation.

Extended Data Fig. 7 Global drought occurrence during 2003-2019.

a, Spatial pattern of the number of droughts during 2003-2019. Droughts are identified as a continuous period when the drought index (ESI) is under a threshold during the growing season (for example, ESI < -0.5; see Methods). b, Average length (black line) and strength (brown line) of droughts aggregated by different f values. Shaded areas present the 25th and the 75th percentiles of the variables.

Extended Data Fig. 8 Averaged year-to-year yield change in response to different drought categories.

Averaged year-to-year yield (measured by maximum greenness, NIRvmax) change in response to different drought categories for a, Maize. b, Rice. c, Soybean. d, Winter wheat during 2003-2019. The black whisker lines represent the 5-95th percentiles from 1000 bootstraps. Whisker lines not crossing 0 indicate that yield deviations during droughts are different than non-droughts at 90% confidence. Light purple and dark purple shades separate bars with f < 36% and f \(\ge\)36%. P-values shown are estimated by using a two-sided t-test comparing the yield deviations in drought vs non-drought years across croplands with f < 36% and f \(\ge\) 36% (that is, in panel a, Maize yields are statistically more sensitive to extremely dry conditions in areas with f \(\ge\) 36%).

Extended Data Fig. 9 Sensitivity of f to the choice of mixing value estimated by AIRS during 2003-2019.

Relative changes in f (%/σ) during the first pentad averaged over different continents when changing a single boundary condition by adding or subtracting standard deviation (denoted as ‘sd’ or ‘σ’) to the mean value for a, \({{\boldsymbol{\delta }}{\boldsymbol{D}}}_{{\boldsymbol{0}}}\) in the free troposphere (618-510hPa). b, \({{\boldsymbol{q}}}_{{\boldsymbol{0}}}\) in the free troposphere. c, \({{\boldsymbol{\delta }}{\boldsymbol{D}}}_{{\boldsymbol{F}}}\) as the surface boundary condition. The whiskers of each marker represent the standard deviation of the change within the aggregated region. GL—global (n = 1230), NA—North America (n = 228), SA—South America (n = 99), EU—Europe (n = 241), AF—Africa (n = 173), AS—Asia (n = 364), AU—Australia (n = 44).

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Jiang, Y., Burney, J.A. Crop water origins and hydroclimate vulnerability of global croplands. Nat Sustain 8, 1491–1504 (2025). https://doi.org/10.1038/s41893-025-01662-1

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