Friedlingstein P, Müller J F, Brasseur G P
Department of Oceanography, Free University of Brussels, CP208, Bld du Triomphe, 1050 Brussels, Belgium.
Environ Pollut. 1994;83(1-2):143-7. doi: 10.1016/0269-7491(94)90032-9.
The biosphere is a major pool in the global carbon cycle; its response to climatic change is therefore of great importance. We developed a 5 degrees x 5 degrees longitude-latitude resolution model of the biosphere in which the global distributions of the major biospheric variables, i.e. the vegetation types and the main carbon pools and fluxes, are determined from climatic variables. We defined nine major broad vegetation types: perennial ice, desert and semi-desert, tundra, coniferous forest, temperate deciduous forest, grassland and shrubland, savannah, seasonal tropical forest and evergreen tropical forest. Their geographical repartition is parameterized using correlations between observed vegetation type, precipitation and biotemperature distributions. The model computes as a function of climate and vegetation type, the variables related to the continental biospheric carbon cycle, i.e. the carbon pools such as the phytomass, the litter and the soil organic carbon; and carbon fluxes such as net primary production, litter production and heterotrophic respiration. The modeled present-day biosphere is in good agreement with observation. The model is used to investigate the response of the terrestrial biosphere to climatic changes as predicted by different General Circulation Models (GCM). In particular, the impact on the biosphere of climatic conditions corresponding to the last glacial climate (LGM), 18 000 years ago, is investigated. Comparison with results from present-day climate simulations shows the high sensitivity of the geographical distribution of vegetation types and carbon content as well as biospheric trace gases emissions to climatic changes. The general trend for LGM compared to the present is an increase in low density vegetation types (tundra, desert, grassland) to the detriment of forested areas, in tropical as well as in other regions. Consequently, the biospheric activity (carbon fluxes and trace gases emissions) was reduced.
生物圈是全球碳循环的一个主要库;因此,它对气候变化的响应至关重要。我们开发了一个5度×5度经纬度分辨率的生物圈模型,其中主要生物圈变量(即植被类型以及主要碳库和碳通量)的全球分布是根据气候变量确定的。我们定义了九种主要的广泛植被类型:常年冰盖、沙漠和半沙漠、苔原、针叶林、温带落叶林、草原和灌木丛、热带稀树草原、季节性热带森林和常绿热带森林。它们的地理分布通过观测到的植被类型、降水量和生物温度分布之间的相关性进行参数化。该模型根据气候和植被类型计算与大陆生物圈碳循环相关的变量,即碳库,如植物生物量、凋落物和土壤有机碳;以及碳通量,如净初级生产力、凋落物产生量和异养呼吸。模拟的现代生物圈与观测结果吻合良好。该模型用于研究陆地生物圈对不同通用环流模型(GCM)预测的气候变化的响应。特别是,研究了对应于18000年前末次冰期气候(LGM)的气候条件对生物圈的影响。与现代气候模拟结果的比较表明,植被类型的地理分布、碳含量以及生物圈微量气体排放对气候变化具有高度敏感性。与当前相比,LGM的总体趋势是低密度植被类型(苔原、沙漠、草原)增加,而热带以及其他地区的森林面积减少。因此,生物圈活动(碳通量和微量气体排放)减少。