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首页> 外文期刊>Global change biology >The net carbon flux due to deforestation and forest re-growth in the Brazilian Amazon: analysis using a process-based model
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The net carbon flux due to deforestation and forest re-growth in the Brazilian Amazon: analysis using a process-based model

机译:巴西亚马逊地区因森林砍伐和森林再生长而产生的净碳通量:使用基于过程的模型进行的分析

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We developed a process-based model of forest growth, carbon cycling and land-cover dynamics named CARLUC (for CARbon and Land-Use Change) to estimate the size of terrestrial carbon pools in terra firme (nonflooded) forests across the Brazilian Legal Amazon and the net flux of carbon resulting from forest disturbance and forest recovery from disturbance. Our goal in building the model was to construct a relatively simple ecosystem model that would respond to soil and climatic heterogeneity that allows us to study the impact of Amazonian deforestation, selective logging and accidental fire on the global carbon cycle. This paper focuses on the net flux caused by deforestation and forest re-growth over the period from 1970 to 1998. We calculate that the net flux to the atmosphere during this period reached a maximum of similar to0.35 PgC yr(-1) (1 PgC= 1 x 10(15) gC) in 1990, with a cumulative release of similar to7 PgC from 1970 to 1998. The net flux is higher than predicted by an earlier study (Houghton et al., 2000) by a total of 1 PgC over the period 1989-1998 mainly because CARLUC predicts relatively high mature forest carbon storage compared with the datasets used in the earlier study. Incorporating the dynamics of litter and soil carbon pools into the model increases the cumulative net flux bysimilar to1 PgC from 1970 to 1998, while different assumptions about land-cover dynamics only caused small changes. The uncertainty of the net flux, calculated with a Monte-Carlo approach, is roughly 35% of the mean value (1 SD).
机译:我们开发了一个基于过程的森林生长,碳循环和土地覆盖动力学模型,名为CARLUC(用于改变碳和土地利用),以估算整个巴西法定亚马逊河(非法定)土地上(非淹没)森林中陆地碳库的大小。森林干扰和森林恢复所产生的碳净通量。我们建立模型的目的是构建一个相对简单的生态系统模型,该模型可以响应土壤和气候异质性,从而使我们能够研究亚马逊森林砍伐,选择性伐木和意外火灾对全球碳循环的影响。本文重点研究了1970年至1998年期间因森林砍伐和森林重新生长而引起的净通量。我们计算得出,在此期间,向大气的净通量达到了约0.35 PgC yr(-1)( 1990年为1 PgC = 1 x 10(15)gC),从1970年到1998年的累积释放量接近7 PgC。净通量比早期研究(Houghton et al。,2000)的预测高。 1989-1998年期间的1 PgC主要是因为CARLUC预测与早期研究中使用的数据集相比,成熟森林的碳储量相对较高。将枯枝落叶和土壤碳库的动力学纳入模型可增加1970年至1998年的累积净通量,接近1 PgC,而关于土地覆被动力学的不同假设只会引起很小的变化。用蒙特卡洛方法计算的净通量的不确定度约为平均值(1 SD)的35%。

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