Vegetation responses to water limitation are difficult to predict owing to large variation across space and time. Our global analysis of soil moisture dynamics reveals that plant water-use strategies vary systematically by ecosystem type in response to recent ecological and climatic conditions.
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References
Kannenberg, S. A. et al. Opportunities, challenges and pitfalls in characterizing plant water-use strategies. Funct. Ecol. 36, 24–37 (2022). This review summarizes various ‘plant water-use strategy’ frameworks.
Trugman, A. T., Medvigy, D., Mankin, J. S. & Anderegg, W. R. L. Soil moisture stress as a major driver of carbon cycle uncertainty. Geophys. Res. Lett. 45, 6495–6503 (2018). This study finds that soil moisture limitation is a key driver of uncertainty in model simulations of the carbon cycle.
Dorigo, W. A. et al. The International Soil Moisture Network: serving Earth system science for over a decade. Hydrol. Earth Syst. Sci. 25, 5749–5804 (2021). This article describes the International Soil Moisture Network, its sites, data and quality control procedures.
Araki, R., Morgan, B. E., McMillan, H. K. & Caylor, K. K. Nonlinear soil moisture loss function reveals vegetation responses to water availability. Geophys. Res. Lett. 52, e2024GL111403 (2025). This study uses satellite data to show that the soil moisture loss function is nonlinear, despite historically being modelled as a linear function.
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This is a summary of: Morgan, B. E. et al. Ecological and hydroclimatic determinants of vegetation water-use strategies. Nat. Ecol. Evol. https://doi.org/10.1038/s41559-025-02810-8 (2025).
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Plant responses to water stress revealed from soil moisture dynamics. Nat Ecol Evol 9, 1765–1766 (2025). https://doi.org/10.1038/s41559-025-02826-0
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DOI: https://doi.org/10.1038/s41559-025-02826-0