Published March 1, 2026 | Version Supplemental material
Journal Article Open

Beyond optimality: Dryland ecosystems infrequently use water efficiently for carbon gain

  • 1. ROR icon Northern Arizona University
  • 2. ROR icon California Institute of Technology
  • 3. ROR icon United States Geological Survey
  • 4. ROR icon University of New Mexico

Abstract

Optimality theory assumes plants maximize carbon gain per unit water lost and is often implemented to scale leaf-level carbon gain and water use to regional and global scales. Optimality theory is often mathematically represented by assuming plant water-use efficiency (WUE) scales with VPDk, where k = ½ represents expected optimal behavior. It is unclear, however, if this relationship holds in arid and semi-arid ecosystems that are strongly impacted by soil and atmospheric moisture status. We used data from seven flux tower sites along an aridity gradient in New Mexico to answer: how does the relationship between WUE and VPD compare to expectations based on optimality theory? To address this question, we integrated the Dynamic Evapotranspiration Partitioning Approach for Rapid Timescales with a stochastic antecedent model to estimate ecosystem-level WUE (GPP/T) and the net sensitivity of WUE to VPD, or kDynamic, which we compare to the theoretical optimal sensitivity of k = ½. Our results show that optimality theory is not always appropriate, and kDynamic often deviates from ½, especially at some of the more arid sites or during periods of low soil moisture. At less arid, higher elevation sites, kDynamic is most consistent with optimality theory at moderate VPD levels, but not at high VPD. In general, the sensitivity of WUE to VPD is highly variable such that kDynamic exhibits notable daily and seasonal variability, suggesting highly dynamic stomatal behavior. These results emphasize that representing plant water-use strategies as dynamic in time and space is critical to improving large-scale estimates of plant water use.

Copyright and License

© 2025 Elsevier B.V. All rights are reserved, including those for text and data mining, AI training, and similar technologies.

Acknowledgement

This research was supported by NSF Hydrologic Sciences award EAR1834699 to K.S‐C., K.O., and M.L., a DOE Ameriflux Management Project award to M.L., a USGS‐NSF Internship Program supplement to award EAR1834699, and NASA FINESST award 80NSSC22K1443 to E.R. and K.O. We would also like to thank Michael Fell for his R functions for summarizing Bayesian output. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government.

Data Availability

All code, models, and data files for the gap-filled flux tower site data and model output used for the analyses in this paper can be found on Github via Zenodo (doi:10.5281/zenodo.15080738).

Supplemental Material

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Additional details

Related works

Is supplemented by
Dataset: 10.5281/zenodo.15080738 (DOI)

Funding

National Science Foundation
EAR-1834699
United States Department of Energy
National Aeronautics and Space Administration
80NSSC22K1443

Dates

Submitted
2025-08-13
Accepted
2025-12-14
Available
2025-12-26
Version of record

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Caltech groups
Division of Geological and Planetary Sciences (GPS)
Publication Status
Published