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Ozone and Climate Change Interact to Affect Streamflow

Photo of Watershed locations in the southern Appalachian states of Tennessee, North Carolina, Virginia, and West Virginia. MB Adams, USDA Forest ServiceWatershed locations in the southern Appalachian states of Tennessee, North Carolina, Virginia, and West Virginia. MB Adams, USDA Forest ServiceSnapshot : Climate change is affecting the Nation's forests, but not in isolation. Tropospheric ozone has long been known to affect the health of individual trees. Recent research by Forest Service scientists and partners shows that ozone and climate change can interact to change how forests use water at the watershed scale.

Principal Investigators(s) :
Adams, Mary Beth 
Research Location : Tennessee;West Virginia;Virginia;North Carolina
Research Station : Northern Research Station (NRS)
Year : 2013
Highlight ID : 487

Summary

The capacity of forests to mitigate global climate change can be negatively influenced by air pollutants-particularly tropospheric ozone, which may impair both photosynthesis and plant transpiration, thus ultimately affecting ecosystem productivity and watershed hydrology. Forest Service and collaborating scientists evaluated individual and interactive effects of ozone and climate on late season stream flow from six forested watersheds in the eastern and southeastern United States, using simulation models. In all cases, including ozone significantly improved the ability of the model to predict water use relative to climate-only models. Effects of ozone and its interactions with climate were consistently negative and varied with actual ozone exposures, both spatially across the region and over time. Conservative estimates of the influence of ozone on the variability of observed flow ranged from 7 percent in the area of lowest ozone exposure in West Virginia to 23 percent in the areas of highest exposure in Tennessee. Despite the frequent assumption that ozone reduces tree water loss, the team's findings provide evidence that ozone at near ambient concentrations can reduce stomatal control of leaf transpiration, thereby increasing water use by forests. These changes could increase the frequency and severity of episodic drought and affect flow-dependent aquatic biota in forested watersheds.

Forest Service Partners

External Partners

  • Ge Sun, Southern Research Station
  • Johan Uddling, University of Gothenburg, Sweden
  • John H. Porter, University of Virginia
  • Neil Pederson, Columbia University Lamont-Doherty Earth Observatory
  • Samuel B. McLaughlin & Patrick J. Mulholland (deceased), Oak Ridge National Laboratory, TN

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