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Can we reconcile differences in estimates of carbon fluxes from land-use change and forestry for the 1990s?

机译:我们能否调和1990年代土地利用变化和林业造成的碳通量估算值的差异?

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The effect of Land Use Change and Forestry (LUCF) on terrestrial carbonfluxes can be regarded as a carbon credit or debit under the UNFCCC, butscientific uncertainty in the estimates for LUCF remains large. Here, weassess the LUCF estimates by examining a variety of models of differenttypes with different land cover change maps in the 1990s. Annual carbonpools and their changes are separated into different components for separategeographical regions, while annual land cover change areas and carbon fluxesare disaggregated into different LUCF activities and the biospheric responsedue to CO2 fertilization and climate change. We developed aconsolidated estimate of the terrestrial carbon fluxes that combinesbook-keeping models with process-based biogeochemical models and inventoryestimates and yields an estimate of the global terrestrial carbon flux thatis within the uncertainty range developed in the IPCC 4th Assessment Report.We examined the USA and Brazil as case studies in order to assess the causeof differences from the UNFCCC reported carbon fluxes. Major differences inthe litter and soil organic matter components are found for the USA.Differences in Brazil result from assumptions about the LUC for agriculturalpurposes. The effects of CO2 fertilization and climate change also varysignificantly in Brazil. Our consolidated estimate shows that the small sinkin Latin America is within the uncertainty range from inverse models, butthat the sink in the USA is significantly smaller than the inverse modelsestimates. Because there are different sources of errors at the countrylevel, there is no easy reconciliation of different estimates of carbonfluxes at the global level. Clearly, further work is required to developdata sets for historical land cover change areas and models ofbiogeochemical changes for an accurate representation of carbon uptake oremissions due to LUC.
机译:根据《联合国气候变化框架公约》,土地使用变化和林业(LUCF)对陆地碳通量的影响可被视为碳信用额或借方,但LUCF估算的科学不确定性仍然很大。在这里,我们通过研究1990年代各种类型的模型和不同的土地覆被变化图来评估LUCF估算。年度碳库及其变化被分为不同的地理区域组成部分,而年度土地覆盖变化区域和碳通量则被分解为不同的LUCF活动和由于CO 2 施肥和气候变化引起的生物圈响应。我们对陆地碳通量进行了综合估算,将簿记模型与基于过程的生物地球化学模型相结合,并进行了库存估算,并得出了全球陆地碳通量的估算值,该估算值在IPCC第四次评估报告中确定的不确定性范围内。以巴西为案例研究,以评估与UNFCCC报告的碳通量差异的原因。美国的凋落物和土壤有机质成分存在主要差异。巴西的差异源自对农业用途LUC的假设。在巴西,CO 2 施肥和气候变化的影响也显着不同。我们的综合估计表明,拉丁美洲的小沉没处于反演模型的不确定性范围内,但美国的沉没明显小于反演模型估计的不确定性。由于国家/地区的错误来源不同,因此全球范围内对碳通量的不同估计值很难轻易核对。显然,需要作进一步的工作来开发历史土地覆盖变化区域的数据集和生物地球化学变化的模型,以准确表示由于土地利用变化而产生的碳吸收量。

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