EGU2020-13465
https://doi.org/10.5194/egusphere-egu2020-13465
EGU General Assembly 2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Emerging mechanisms of ecosystem functioning in a warmer and drier world

José M. Grünzweig1, Hans J. De Boeck2, Ana Rey3, Omer Tzuk4, Ehud Meron4,5, Omar Flores3, Maria J. Santos6, and Michael Bahn7
José M. Grünzweig et al.
  • 1Hebrew University of Jerusalem, Institute of Plant Sciences and Genetics in Agriculture, Faculty of Agriculture, Food and Environment, Rehovot, Israel (jose.gruenzweig@mail.huji.ac.il)
  • 2Plants and Ecosystems, Department of Biology, Universiteit Antwerpen, Wilrijk, Belgium
  • 3Department of Biogeography and Global Change, National Museum of Natural History, Spanish Scientific Council (CSIC), C/Serrano 115bis, 28006 Madrid, Spain
  • 4Department of Physics, Ben-Gurion University, Beer Sheva, 84105, Israel
  • 5Department of Solar Energy and Environmental Physics, Blaustein Institutes for Desert Research, Ben-Gurion University of the Negev, Sede Boqer Campus 84990, Israel
  • 6University Research Priority Program in Global Change and Biodiversity and Department of Geography, University of Zurich, Switzerland
  • 7Department of Ecology, University of Innsbruck, Sternwartestr. 15, 6020 Innsbruck, Austria

Ecosystems are expected to face a significantly warmer and drier climate in the coming decades. Experiments have tried to unravel drought responses of ecosystems in mesic and humid biomes, but the structure and functioning of these systems may change when climatic regime shifts occur. Here, we summarize major mechanisms typical of drylands and indicate how these may come into play when current mesic ecosystems face tipping points in a warmer and drier world.

These dryland mechanisms of ecosystem functioning encompass (i) processes of vegetation development, such as self-organization of vegetation patchiness and formation of biological soil crust, (ii) biologically driven biogeochemical and physiological processes, such as drying-wetting cycles and hydraulic redistribution, and (iii) abiotically driven biogeochemical processes, such as photochemical degradation of organic matter and soil hydrophobicity. We present insights from published studies and original model simulations and mapping, and formulate hypotheses on thresholds and spatial locations beyond which dryland mechanisms are expected to operate in non-xeric ecosystems. Notably, for dryland mechanisms to get activated elsewhere there is no need for non-xeric biomes to become actual drylands. With a globally increasing area exposed to gradually rising temperatures, moderate decline in precipitation, and increasing frequency, duration and intensity of extreme heat and drought events, we envision that dryland mechanisms will increasingly control ecosystem functioning in many regions of the world.

How to cite: Grünzweig, J. M., De Boeck, H. J., Rey, A., Tzuk, O., Meron, E., Flores, O., Santos, M. J., and Bahn, M.: Emerging mechanisms of ecosystem functioning in a warmer and drier world , EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-13465, https://doi.org/10.5194/egusphere-egu2020-13465, 2020

Display materials

Display file