2020 ESA Annual Meeting (August 3 - 6)

COS 130 Abstract - Terrestrial ecosystems vary globally in response to one-year of extreme drought

Kate Wilkins1, Laureano A. Gherardi2, Peter Wilfahrt3, Martin Holdrege4, Scott Collins5, Jeffrey S. Dukes6, Alan Knapp7, Richard Phillips8, Osvaldo Sala2 and Melinda Smith7, (1)Department of Biology, Colorado State University, Fort Collins, CO, (2)School of Life Sciences, Arizona State University, Tempe, AZ, (3)Disturbance Ecology, University of Bayreuth, Bayreuth, Germany, (4)Department of Wildland Resources and the Ecology Center, Utah State University, Logan, UT, (5)Department of Biology, University of New Mexico, Albuquerque, NM, (6)Purdue Climate Change Research Center, Purdue University, West Lafayette, IN, (7)Graduate Degree Program in Ecology, Colorado State University, Fort Collins, CO, (8)Department of Biology, Indiana University, Bloomington, IN
Background/Question/Methods

Climate models predict more frequent, extreme, and spatially extensive droughts in the future, and drought impacts to terrestrial ecosystems have increased globally over the last century. Given the potential for intensified droughts to damage ecosystems and degrade the land carbon sink, there is a pressing scientific and societal imperative to better understand their impacts on terrestrial ecosystems. To prepare for such events, we need to understand how different ecosystems will respond to drought and the mechanisms that drive drought responses across ecosystems.

Our research explores whether global terrestrial ecosystems vary in their response to one year of extreme drought (1 in 100 year event). Specifically, we assess how one year of extreme drought affects aboveground net primary productivity (ANPP) and drought sensitivity—measured as the difference in ANPP between drought and control plots divided by the difference in precipitation received by drought and control plots. Based on the Huxman-Smith model, we expected ecosystems with higher mean annual precipitation (MAP) to be less sensitive to one year of extreme drought than ecosystems with lower MAP. To test this hypothesis, we synthesized a global dataset from the Drought-Net Research Coordination Network’s International Drought Experiment (IDE), which consists of 112 sites from 24 countries and 6 continents.

Results/Conclusions

On average, terrestrial ecosystems exhibited a negative ANPP response to one year of extreme drought, with grassland ecosystems exhibiting more negative responses in ANPP than forest ecosystems. Drought sensitivity also decreased and was less variable with increasing mean annual precipitation. Thus, our study found that terrestrial ecosystems vary substantially in their response to extreme 1-year drought. In addition, our results provide support for the Huxman-Smith model by demonstrating that water-limited terrestrial ecosystems display greater sensitivity to extreme, short-term drought than those that are less water-limited. These findings have important implications as arid ecosystems, which are important drivers of variability in the global carbon cycle, are expected to be more vulnerable to intensified drought than more mesic ecosystems.