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Effects of changes in CO2, climate, and land use on the carbon balance of the land biosphere during the 21st century

机译:二氧化碳,气候和土地利用变化对21世纪陆地生物圈碳平衡的影响

摘要

We studied the effects of climate and land-use change on the global terrestrial carbon cycle for the 21st century. Using the process-based land biosphere model (LPJmL), we mechanistically simulated carbon dynamics for natural and managed lands (agriculture and forestry) and for land-use change processes. We ran LPJmL with twelve different dynamic land-use patterns and corresponding climate and atmospheric CO2 projections. These input data were supplied from the IMAGE 2.2 implementations of the IPCC-SRES storylines for the A2, B1, and B2 scenarios. Each of these SRES scenarios was implemented under four different assumptions on spatial climate patterns in IMAGE 2.2, resulting in twelve different Earth System projections. Our selection of SRES scenarios comprises deforestation and afforestation scenarios, bounding a broad range of possible land-use change. Projected land-use change under different socio-economic scenarios has profound effects on the terrestrial carbon balance: While climate change and CO2 fertilization cause an additional terrestrial carbon uptake of 105-225 PgC, land-use change causes terrestrial carbon losses of up to 445 PgC by 2100, dominating the terrestrial carbon balance under the A2 and B2 scenarios. Our results imply that the potential positive feedback of the terrestrial biosphere on anthropogenic climate change will be strongly affected by land-use change. Spatiotemporally explicit projections of land-use change and the effects of land management on terrestrial carbon dynamics need additional attention in future research.
机译:我们研究了气候和土地利用变化对21世纪全球陆地碳循环的影响。使用基于过程的土地生物圈模型(LPJmL),我们以机械方式模拟了自然和受管理土地(农业和林业)以及土地用途变更过程的碳动态。我们使用十二种不同的动态土地利用模式以及相应的气候和大气CO2预测运行了LPJmL。这些输入数据是从IPCC-SRES故事情节的IMAGE 2.2实现为A2,B1和B2场景提供的。这些SRES情景中的每一个都是在IMAGE 2.2中针对空间气候模式的四种不同假设下实施的,从而产生了十二种不同的地球系统预测。我们选择的SRES情景包括森林砍伐和绿化情景,限制了各种可能的土地利用变化。在不同的社会经济情景下,预计的土地利用变化将对陆地碳平衡产生深远影响:虽然气候变化和CO2施肥导致陆地碳吸收增加了105-225 PgC,但土地利用变化导致陆地碳损失高达445 PgC到2100年,在A2和B2情景下主导了陆地碳平衡。我们的结果表明,陆地生物圈对人为气候变化的潜在积极反馈将受到土地利用变化的强烈影响。土地利用变化的时空明确预测以及土地管理对陆地碳动态的影响在未来的研究中需要进一步关注。

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