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AGU: Journal of Geophysical Research, Biogeosciences

 

Keywords

  • arctic tundra
  • biomass
  • climate gradient
  • patterned-ground
  • vegetation patterns

Index Terms

  • Biogeosciences: Plant ecology
  • Biogeosciences: Permafrost, cryosphere, and high-latitude processes
  • Biogeosciences: Ecosystems, structure and dynamics
  • Cryosphere: Tundra
  • Geographic Location: Arctic region
Abstract
Cited By (5)
 

Abstract

JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 113, G03S02, 11 PP., 2008
doi:10.1029/2007JG000555

Phytomass patterns across a temperature gradient of the North American arctic tundra

Howard E. Epstein

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

Donald A. Walker

Alaska Geobotany Center, Institute of Arctic Biology, University of Alaska Fairbanks, Fairbanks, Alaska, USA

Martha K. Raynolds

Alaska Geobotany Center, Institute of Arctic Biology, University of Alaska Fairbanks, Fairbanks, Alaska, USA

Gensuo J. Jia

Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, China

Alexia M. Kelley

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

Only a few studies to date have collectively examined the vegetation biomass and production of arctic tundra ecosystems and their relationships to broadly ranging climate variables. An additional complicating factor for studying vegetation of arctic tundra is the high spatial variability associated with small patterned-ground features, resulting from intense freeze-thaw processes. In this study, we sampled and analyzed the aboveground plant biomass components of patterned-ground ecosystems in the Arctic of northern Alaska and Canada along an 1800-km north-south gradient that spans approximately 11°C of mean July temperatures. Vegetation biomass was analyzed as functions of the summer warmth index (SWI–sum of mean monthly temperatures > 0°C). The total absolute biomass (g m−2) and biomass of shrubs increased monotonically with SWI, however, biomass of nonvascular species (mosses and lichens), were a parabolic function of SWI, with greatest values at the ends of the gradient. The components of plant biomass on patterned-ground features (i.e., on nonsorted circles or within small polygons) were constrained to a greater degree with colder climate than undisturbed tundra, likely due to the effect of frost heave disturbances on the vegetation. There were also clear differences in the relative abundances of vascular versus nonvascular plants on and off patterned-ground features along the SWI gradient. The spatial patterns of biomass differ among plant functional groups and suggest that plant community responses to temperature, and land-surface processes that produce patterned-ground features, are quite complex.

Received 19 July 2007; accepted 17 January 2008; published 6 May 2008.

Citation: Epstein, H. E., D. A. Walker, M. K. Raynolds, G. J. Jia, and A. M. Kelley (2008), Phytomass patterns across a temperature gradient of the North American arctic tundra, J. Geophys. Res., 113, G03S02, doi:10.1029/2007JG000555.

Cited By

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