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Redistribution of forest biomass in an heterogeneous environment of subtropical Andes undergoing agriculture adjustment

机译:亚热带安第斯山脉异质环境中进行农业调整的森林生物量再分配

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Estimations of the carbon stored in the above-ground biomass are important from traditional, ecological and forestry to contemporary climate and land-use change perspectives. Carbon sequestration and storage is reduced by deforestation and degradation and enhanced by forest regrowth and expansion. Recent studies show that forests are experiencing redistribution at different scales. Regions with steep topographical gradients simultaneously experience these four processes, upon which the final carbon balance in forests depends, but large scale patterns of above-ground carbon changes within forests have generally been overlooked. We developed above-ground carbon maps for 2000 and 2012 in a heterogeneous environment of subtropical Andes to a) explore the patterns of change in relation to biophysical variables and forests types and b) calculate the relative contribution of within forest carbon change and of forest expansion/deforestation to total above-ground carbon balance. Above-ground carbon trends showed spatial variation: biomass losses occurred in dry forests at low-mid elevations, while gains were restricted to higher elevation forests. Within forest changes implied larger changes in carbon stocks (+361976 Mg C) and in an opposite direction than deforestation and reforestation (-56750.16 Mg C), and determined an overall stability in terms of above-ground carbon for the study period. These contrasting patterns of above-ground change may be representative of larger heterogeneous regions such as tropical and subtropical Andes, and highlight the need of explicitly accounting for within forests change in current carbon regional balances. (C) 2015 Elsevier Ltd. All rights reserved.
机译:从传统,生态和林业到当代气候和土地利用变化的观点,估算地上生物量中储存的碳非常重要。砍伐森林和退化减少了碳的固存和储存,而森林的再生和扩张则增加了碳的封存和储存。最近的研究表明,森林正在经历不同规模的再分配。具有陡峭地形坡度的区域同时经历了这四个过程,森林的最终碳平衡取决于这四个过程,但是通常忽略了森林内地上碳变化的大规模模式。我们在亚热带安第斯山脉的异质环境中绘制了2000年和2012年的地上碳图,以a)探索与生物物理变量和森林类型有关的变化模式,以及b)计算森林内部碳变化和森林扩展的相对贡献/砍伐森林以达到地上总碳平衡。地上碳趋势显示出空间变化:生物量损失发生在中低海拔的干旱森林中,而增加仅限于海拔较高的森林。在森林内变化意味着碳储量的更大变化(+361976 Mg C),并且方向与毁林和再造林(-56750.16 Mg C)相反,并确定了研究期内地上碳的总体稳定性。这些相反的地上变化模式可能代表较大的非均质区域,例如热带和亚热带安第斯山脉,并强调需要明确说明森林内当前碳区域平衡的变化。 (C)2015 Elsevier Ltd.保留所有权利。

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