Eve-Lyn Hinckley (CU Boulder)
There is increasing evidence that air temperature is rising faster in high elevation mountain landscapes versus lowland regions. While globally, climate warming occurs at an average rate of 0.2 ± 0.1 °C / decade, high elevation regions are warming on average 0.3°C ± 0.3 °C / decade. Predicting how mountain landscapes will change in response to climate forcings is complicated by spatial variability of the alpine critical zone, including microtopographical gradients that lead to differences in soil properties (e.g., moisture, temperature, depth, and organic matter content), which in turn affect biogeochemical cycling, we well as the composition and abundance of plant communities and wildlife over short length scales. In this talk, I will share results of several recent studies at the Niwot Ridge Long-term Ecological Research (LTER) site in the Colorado Rocky Mountains, U.S., that provide insight into how climate-driven changes in the alpine critical zone are affecting the cycling of carbon (C), nitrogen (N), sulfur (S), and heavy metals, as well as the timing and degree to which the landscape is hydrologically connected during the year. Recent data indicate that even as air quality regulation has decreased the inputs of oxidized N and S, unregulated atmospheric deposition of ammonium-N is on the rise, the thawing of subsurface ice features is changing the timing and amounts of surface water flows, and losses of these and other ice features is increasing export of sulfate to surface water. Wetter portions of the landscape are now accumulating C, N, and S, and have become hotspots of methylmercury production—a neurotoxin that bioaccumulates and biomagnifies in the food web. Together, these studies provide an emergent picture of how high elevation mountain landscapes are changing under a warming climate and other anthropogenic pressures, the cascade of consequences for critical zone processes, and the issues that we must quickly confront to mitigate their loss globally.
Eve-Lyn Hinckley is an Associate Professor of Ecology and Evolutionary Biology and Fellow of the Cooperative Institute for Research in Environmental Sciences at the University of Colorado, Boulder. Her research focuses on studying the elements that underlie all life on Earth, with an emphasis on how they are changed by human activities and how those changes feed back to affect human welfare. Dr. Hinckley earned her Ph.D. in Geological and Environmental Sciences from Stanford University, and B.A. in Environmental Studies from Middlebury College. Her research on modern changes to the global sulfur cycle is supported by multiple funding agencies, including the prestigious CAREER program through The U.S. National Science Foundation, a grant from U.S. Department of Agriculture, and the National Geographic Society. Dr. Hinckley has been recognized as a University of Colorado Research & Innovation Office Faculty Fellow and Arts & Sciences Support of Education Through Technology Teaching Fellow.
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