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AGU: Journal of Geophysical Research, Biogeosciences

 

Keywords

  • arctic tundra
  • climate change
  • hydrology
  • modeling
  • nonsorted circles
  • vegetation

Index Terms

  • Cryosphere: Active layer
  • Cryosphere: Periglacial processes
  • Global Change: Cryospheric change
  • Hydrology: Vadose zone
Abstract
Cited By (0)
 

Abstract

Simulating nonsorted circle development in arctic tundra ecosystems

Ronald P. Daanen

Permafrost Laboratory, Geophysical Institute, University of Alaska Fairbanks, Fairbanks, Alaska, USA

Debasmita Misra

Department of Mining and Geological Engineering, College of Engineering and Mines, University of Alaska Fairbanks, Fairbanks, Alaska, USA

Howard Epstein

Department of Environmental Sciences, University of Virginia, Charlottesville, Virginia, USA

Donald Walker

Department of Biology and Wildlife, University of Alaska Fairbanks, Fairbanks, Alaska, USA

Vladimir Romanovsky

Permafrost Laboratory, Geophysical Institute, University of Alaska Fairbanks, Fairbanks, Alaska, USA

Nonsorted circles, ubiquitous to the Arctic Tundra region, are patterned ground features with circular semibarren areas surrounded by vegetation. These circles are formed and persist as an ecosystem due to complex soil-water-energy-ice-plant relationships and dynamics in the Arctic. In this paper, we present the first model that captures the dynamics of the physical and biological components of the nonsorted circle ecosystem in order to understand its formation and persistence, especially in a changing climatic environment. We have applied a coupled model describing (1) vegetation dynamics (ArcVeg) and (2) coupled heat and moisture transport with phase change (WIT) in the active layer of the soil where such circles are initiated and developed. We simulated the system behavior during the formation process starting with a random vegetation development. The vegetation provided heterogeneous insulation to the soil surface. During freezing, the noninsulated areas froze first, resulting in preferential ice accumulation in those areas. The ice prevented the vegetation from developing further in those areas and thus developed and stabilized the nonsorted circle pattern. The model produced a nonsorted circle pattern that was well compared to those observed in the field. The model also illustrated that the availability of water was critical for the sustenance and stability of the nonsorted circle. The effect of climatic variations on the freezing process on the other hand did not seem to affect the formation and sustenance of nonsorted circles.

Received 2 January 2008; accepted 15 April 2008; published 15 July 2008.

Citation: Daanen, R. P., D. Misra, H. Epstein, D. Walker, and V. Romanovsky (2008), Simulating nonsorted circle development in arctic tundra ecosystems, J. Geophys. Res., 113, G03S06, doi:10.1029/2008JG000682.

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