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JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 108, NO. D19, 8171, doi:10.1029/2002JD002559, 2003

Climate change and Arctic ecosystems: 2. Modeling, paleodata-model comparisons, and future projections

J. O. Kaplan

Max Planck Institute for Biogeochemistry, Jena, Germany


N. H. Bigelow

Alaska Quaternary Center, University of Alaska, Fairbanks, Alaska, USA


I. C. Prentice

Max Planck Institute for Biogeochemistry, Jena, Germany


S. P. Harrison

Max Planck Institute for Biogeochemistry, Jena, Germany
Dynamic Paleoclimatology, Lund University, Lund, Sweden


P. J. Bartlein

Department of Geography, University of Oregon, Eugene, Oregon, USA


T. R. Christensen

Climate Impacts Group, Department of Ecology, Lund University, Lund, Sweden


W. Cramer

Potsdam Institute for Climate Impact Research, Potsdam, Germany


N. V. Matveyeva

Department of Vegetation of the Far North, Komarov Botanical Institute, St. Petersburg, Russia


A. D. McGuire

U.S. Geological Survey, Alaska Cooperative Fish and Wildlife Research Unit, University of Alaska, Fairbanks, Alaska, USA


D. F. Murray

University of Alaska Museum, Fairbanks, Alaska, USA


V. Y. Razzhivin

Department of Vegetation of the Far North, Komarov Botanical Institute, St. Petersburg, Russia


B. Smith

Max Planck Institute for Biogeochemistry, Jena, Germany
Climate Impacts Group, Department of Ecology, Lund University, Lund, Sweden


D. A. Walker

Institute of Arctic and Alpine Research, University of Colorado, Boulder, Colorado, USA
Institute of Arctic Biology, University of Alaska, Fairbanks, Alaska, USA


P. M. Anderson

Quaternary Research Center, University of Washington, Seattle, Washington, USA


A. A. Andreev

Alfred Wegner Institute for Polar and Marine Research, Forschungsstelle Potsdam, Potsdam, Germany


L. B. Brubaker

College of Forest Resources, University of Washington, Seattle, Washington, USA


M. E. Edwards

Institute of Arctic Biology, University of Alaska, Fairbanks, Alaska, USA
Department of Geography, Norges Teknisk-Naturvitenskapelige Universitet, Trondheim, Norway


A. V. Lozhkin

Northeast Interdisciplinary Scientific Research Institute, Russian Academy of Sciences, Magadan, Russia


Abstract

Large variations in the composition, structure, and function of Arctic ecosystems are determined by climatic gradients, especially of growing-season warmth, soil moisture, and snow cover. A unified circumpolar classification recognizing five types of tundra was developed. The geographic distributions of vegetation types north of 55°N, including the position of the forest limit and the distributions of the tundra types, could be predicted from climatology using a small set of plant functional types embedded in the biogeochemistry-biogeography model BIOME4. Several palaeoclimate simulations for the last glacial maximum (LGM) and mid-Holocene were used to explore the possibility of simulating past vegetation patterns, which are independently known based on pollen data. The broad outlines of observed changes in vegetation were captured. LGM simulations showed the major reduction of forest, the great extension of graminoid and forb tundra, and the restriction of low- and high-shrub tundra (although not all models produced sufficiently dry conditions to mimic the full observed change). Mid-Holocene simulations reproduced the contrast between northward forest extension in western and central Siberia and stability of the forest limit in Beringia. Projection of the effect of a continued exponential increase in atmospheric CO2 concentration, based on a transient ocean-atmosphere simulation including sulfate aerosol effects, suggests a potential for larger changes in Arctic ecosystems during the 21st century than have occurred between mid-Holocene and present. Simulated physiological effects of the CO2 increase (to >700 ppm) at high latitudes were slight compared with the effects of the change in climate.

Received 23 May 2002; accepted 29 January 2003; published 8 October 2003.

Index Terms: 0315 Atmospheric Composition and Structure: Biosphere/atmosphere interactions; 1615 Global Change: Biogeochemical processes (4805); 1620 Global Change: Climate dynamics (3309); 1851 Hydrology: Plant ecology.


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Citation: Kaplan, J. O., et al. (2003), Climate change and Arctic ecosystems: 2. Modeling, paleodata-model comparisons, and future projections, J. Geophys. Res., 108(D19), 8171, doi:10.1029/2002JD002559.