4.8 Article

Rapid increases in shrubland and forest intrinsic water-use efficiency during an ongoing megadrought

Publisher

NATL ACAD SCIENCES
DOI: 10.1073/pnas.2118052118

Keywords

climate change; drought; iWUE; stable isotopes; tree rings

Funding

  1. NSF Division of Environmental Biology (DEB) grants [1950025, 1754430]
  2. NSF DEB Grant [1950025, 1753845, 1714972, 1802880, 2003017]
  3. US Department of Agriculture (USDA) Forest Service Forest Health Protection Evaluation Monitoring program [19-05]
  4. US Department of Energy Environmental System Science program [DOE DE-SC0022052]
  5. David and Lucille Packard Foundation
  6. USDA National Institute of Food and Agriculture, Agricultural and Food Research Initiative Competitive Program, Ecosystem Services and Agro-Ecosystem Management Grant [2018-67019-27850]
  7. Direct For Biological Sciences
  8. Division Of Environmental Biology [1950025, 1753845] Funding Source: National Science Foundation
  9. Division Of Environmental Biology
  10. Direct For Biological Sciences [1754430] Funding Source: National Science Foundation
  11. U.S. Department of Energy (DOE) [DE-SC0022052] Funding Source: U.S. Department of Energy (DOE)

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Globally, intrinsic water-use efficiency (iWUE) has shown a significant increase over the past century in line with rising atmospheric CO2 concentrations. Recent drying trends in the American Southwest have led to a rapid increase in iWUE in shrub species in the region, surpassing that of tree species. While a shift towards more water-efficient vegetation may benefit plant health, ongoing trends of lower plant density, diminished growth, and increasing vegetation mortality in the Southwest suggest that this increase in iWUE is unlikely to offset the negative impacts of aridification.
Globally, intrinsic water-use efficiency (iWUE) has risen dramatically over the past century in concert with increases in atmospheric CO2 concentration. This increase could be further accelerated by long-term drought events, such as the ongoing multidecadal megadrought in the American Southwest. However, direct measurements of iWUE in this region are rare and largely constrained to trees, which may bias estimates of iWUE trends toward more mesic, high elevation areas and neglect the responses of other key plant functional types such as shrubs that are dominant across much of the region. Here, we found evidence that iWUE is increasing in the Southwest at one of the fastest rates documented due to the recent drying trend. These increases were particularly large across three common shrub species, which had a greater iWUE sensitivity to aridity than Pinus ponderosa, a common tree species in the western United States. The sensitivity of both shrub and tree iWUE to variability in atmospheric aridity exceeded their sensitivity to increasing atmospheric [CO2]. The shift to more water-efficient vegetation would be, all else being equal, a net positive for plant health. However, ongoing trends toward lower plant density, diminished growth, and increasing vegetation mortality across the Southwest indicate that this increase in iWUE is unlikely to offset the negative impacts of aridification.

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