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A. Ganopolski, S. Rahmstorf, V. Petoukhov, M. Claussen (1998)
Simulation of modern and glacial climates with a coupled global model of intermediate complexityNature, 391
K. Shine (2000)
Radiative Forcing of Climate ChangeSpace Science Reviews, 94
D. Hoyt, K. Schatten (1993)
A discussion of plausible solar irradiance variations, 1700-1992Journal of Geophysical Research, 98
R. Houghton, J. Hobbie, J. Melillo, B. Moore, B. Peterson, G. Shaver, G. Woodwell (1983)
Changes in the Carbon Content of Terrestrial Biota and Soils between 1860 and 1980: A Net Release of CO"2 to the AtmosphereEcological Monographs, 53
(1993)
Climate Dynamics, in press
D. Rind (1996)
The Potential for Modeling the Effects of Different Forcing Factors on Climate During the Past 2000 Years
R. Pielke, .. Sr, R. Avissar, M. Raupach, A. Dolman, X. Zeng, A. Denning (1998)
Interactions between the atmosphere and terrestrial ecosystems: influence on weather and climateGlobal Change Biology, 4
D. Fisk (1988)
The boreal forest
J. Foley, S. Levis, I. Prentice, D. Pollard, S. Thompson (1998)
Coupling dynamic models of climate and vegetationGlobal Change Biology, 4
V. Brovkin, A. Ganopolski, Y. Svirezhev (1997)
A continuous climate-vegetation classification for use in climate-biosphere studiesEcological Modelling, 101
G. Thomas, P. Rowntree (1992)
The Boreal Forests and ClimateQuarterly Journal of the Royal Meteorological Society, 118
E. Dickinson, A. Henderson‐sellers, J. Kennedy (1993)
Biosphere-atmosphere transfer scheme(BATS) version 1e as coupled to the NCAR community climate model
G. Bonan, D. Pollard, S. Thompson (1992)
Effects of boreal forest vegetation on global climateNature, 359
Xinyu Zheng, E. Eltahir (1997)
The response to deforestation and desertification in a model of West African monsoonsGeophysical Research Letters, 24
U. Cubasch, R. Voss, G. Hegerl, J. Waszkewitz, T. Crowley (1997)
Simulation of the influence of solar radiation variations on the global climate with an ocean-atmosphere general circulation modelClimate Dynamics, 13
A. Ganopolski, C. Kubatzki, M. Claussen, V. Brovkin, V. Petoukhov (1998)
The influence of vegetation-atmosphere-ocean interaction on climate during the mid-holoceneScience, 280 5371
(1997)
ff ects of land use on the climate of scale temperature patterns and climate forcing over the the United States . Climatic Change , 37 , 449 – 486 . past six centuries
M. Wilson, A. Henderson‐sellers (1985)
A global archive of land cover and soils data for use in general circulation climate modelsInternational Journal of Climatology, 5
S. Chalita, H. Treut (1994)
The albedo of temperate and boreal forest and the Northern Hemisphere climate: a sensitivity experiment using the LMD GCMClimate Dynamics, 10
(1999)
The impact of land use on the climate Mauna Loa Observatory, Hawaii, 1958–93
S. Levis, J. Foley, V. Brovkin, D. Pollard (1999)
On the stability of the high-latitude climate-vegetation system in a coupled atmosphere-biosphere modelGlobal Ecology and Biogeography, 8
G. Bonan (1997)
Effects of Land Use on the Climate of the United StatesClimatic Change, 37
M. Mann, R. Bradley, M. Hughes (1998)
Global-scale temperature patterns and climate forcing over the past six centuriesNature, 392
(1992)
ff ects system in a coupled atmosphere - biosphere model . Global of boreal forest vegetation on global climate
In order to estimate the effect of historical land cover change (deforestation) on climate, we perform a set of experiments with a climate system model of intermediate complexity – CLIMBER‐2. We focus on the biophysical effect of the land cover change on climate and do not explicitly account for the biogeochemical effect. A dynamic scenario of deforestation during the last millennium is formulated based on the rates of land conversion to agriculture. The deforestation scenario causes a global cooling of 0.35 °C with a more notable cooling of the northern hemisphere (0.5 °C). The cooling is most pronounced in the northern middle and high latitudes, especially during the spring season. To compare the effect of deforestation on climate with other forcings, climate responses to the changing atmospheric CO2 concentration and solar irradiance are also analysed. When all three factors are taken into account, dynamics of northern hemisphere temperature during the last 300 years within the model are generally in agreement with the observed (reconstructed) temperature trend. We conclude that the impact of historical land cover changes on climate is comparable with the impact of the other climate forcings and that land cover forcing is important for reproducing historical climate change.
Global Ecology and Biogeography – Wiley
Published: Nov 1, 1999
Keywords: ; ; ; ; ; ; ; ;
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