Sensitivity of terrestrial carbon storage to CO2-induced climate change: Comparison of four scenarios based on general circulation models
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Abstract
The potential impacts of CO2-induced climate change on terrestrial carbon storage was estimated using the Holdridge Life-Zone Classification and four climate change scenarios derived from general circulation models. Carbon values were assigned to life-zones and their associated soils from published studies. All four scenarios suggest an increase in area occupied by forests although details of predicted patterns vary among the scenarios. There is a poleward shift of the forested zones, with an increase in the areal extent of tropical forests and a shift of the boreal forest zone into the region currently occupied by tundra. Terrestrial carbon storage increased from 0.4% (8.5 Gt) to 9.5% (180.5 Gt) above estimates for present conditions. These changes represent a potential reduction of 4 to 85 ppm on elevated atmospheric CO2 levels.
Keywords
Present Condition Tropical Forest General Circulation Model Potential Reduction Boreal ForestPreview
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References
- Akima, H.: 1978, ‘A Method of Bivariate Interpolation and Smooth Surface Fitting for Irregular Disturbed Datapoints’, ACM Trans. Math. Software 4, 148–159.Google Scholar
- Box, E. O.: 1980, Macroclimate and Plant Forms: An Introduction to Predictive Modeling in Phytogeography, Junk, The Hague.Google Scholar
- Emanuel, W. R., Shugart, H. H. and Stevenson, M. P.: 1985, ‘Climatic Change and the Broad-Scale Distribution of Terrestrial Ecosystem Complexes’, Climatic Change 7, 29–43.Google Scholar
- Green, P. J. and Sibson, R.: 1978, ‘Computing Dirichlet Tessellations in the Plane’, The Computer Journal 21, 168–173.Google Scholar
- Hansen, J., Lacis, A., Rind, D., Russell, G., Stone, P., Fung, I., Reudy, R. and Lerner, J.: 1984, ‘Climate Sensitivity: Analysis of Feedback Mechanisms’, in Hansen, J. and Thompson, R. (eds.), Geophysical Monogr. 29, American Geophysical Union, Washington, D.C.Google Scholar
- Hansen, J., Fung, I., Lacis, A., Rind, D., Russell, G., Lebedeff, S., Reudy, R. and Stone, P.: 1988, ‘Global Climate Changes as Forecast by the GISS-3-D Model’, J. Geophys. Res. 93, 9341–9364.Google Scholar
- Holdridge, L. R.: 1959, ‘Simple Method for Determining Potential Evapotranspiration from Temperature Data’, Science 130, 572.Google Scholar
- Holdridge, L. R.: 1967, Life Zone Ecology, Tropical Science Center, San Jose.Google Scholar
- Lashof, D. A.: 1987, The Role of the Biosphere in the Global Carbon Cycle: Evaluating Through Biospheric Modeling and Atmospheric Measurement, Ph.D. dissertation, University of California, Berkeley.Google Scholar
- Leemans, R. and Cramer, W.: 1990, ‘The IIASA Climate Database for Land Area on a Grid of 0.5° Resolution’, WP-41, International Institute for Applied Systems Analysis, Laxenburg.Google Scholar
- Manabe, S. and Stouffer, R. J.: 1980, ‘Sensitivity of a Global Climate Model to an Increase in CO2 Concentration in the Atmosphere’, J. Geophys. Res. 85, 5529–5554.Google Scholar
- Manabe, S. and Wetherald, R. T.: 1987, ‘Large Scale Changes in Soil Wetness Induced by an Increase in Carbon Dioxide’, J. Atm. Sci. 44, 1211–1235.Google Scholar
- Mitchell, J. F. B.: 1983, ‘The Seasonal Response of a General Circulation Model to Changes in CO2 and Sea Temperatures’, Q. J. Roy. Met. Soc. 109, 113–152.Google Scholar
- Olson, J. S., Watts, J. A. and Allison, L. J.: 1983, ‘Carbon in Live Vegetation of Major World Ecosystems’, ESD Pub. No. 1997, Oak Ridge National Laboratory, TN.Google Scholar
- Post, W. M., Emanuel, W. R., Zinke, P. J. and Stangenberger, A. G.: 1982, ‘Soil Carbon Pools and World-Life Zones’, Nature 298, 156–159.Google Scholar
- Prentice, K. C. and Fung, I. Y.: 1990, ‘Bioclimatic Simulations Test the Sensitivity of Terrestrial Carbon Storage to Perturbed Climates’, Nature 346, 48–51.Google Scholar
- Prentice, K. C.: 1990, ‘Bioclimatic Distribution of Vegetation for GCM Studies’, J. Geophys. Res. (in press).Google Scholar
- Schlesinger, M. and Zhao, Z.: 1988, ‘Seasonal Climatic Changes Induced by Doubled CO2 as Simulated by the OSU Atmospheric GCM/Mixed Layer Ocean Model’, Oregon St. U, Corvallis, OR, Climate Research Institute.Google Scholar
- Sedjo, R. A. and Solomon, A. M.: 1989, ‘Climate and Forests’, in Rosenberg, N. J., Easterling, W. E., Crosson, P. R. and Darmstadter, J. (eds.), Greenhouse Warming: Abatement and Adaptation, Resources For The Future, Washington, D.C.Google Scholar
- Washington, W. and Meehl, J.: 1984, ‘Seasonal Cycle Experiments on the Climate Sensitivity due to a Doubling of CO2 with an Atmospheric General Circulation Model Coupled to a Simple Mixed Layer Ocean Model’, J. Geophys. Res. 89, 9475–9503.Google Scholar
- Wetherald, R. and Manabe, S.: 1986, ‘An Investigation of Cloud Cover Change in Response to Thermal Forcing’, Climatic Change 8, 5–23.Google Scholar