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Audit of the global carbon budget: estimate errors and their impact on uptake uncertainty

机译:全球碳预算审计:估计误差及其对吸收不确定性的影响

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Over the last 5 decades monitoring systems have been developed to detect changes in the accumulation of carbon (C) in the atmosphere and ocean; however, our ability to detect changes in the behavior of the global C cycle is still hindered by measurement and estimate errors. Here we present a rigorous and flexible framework for assessing the temporal and spatial components of estimate errors and their impact on uncertainty in net C uptake by the biosphere. We present a novel approach for incorporating temporally correlated random error into the error structure of emission estimates. Based on this approach, we conclude that the 2 sigma uncertainties of the atmospheric growth rate have decreased from 1.2 Pg C yr(-1) in the 1960s to 0.3 Pg C yr(-1) in the 2000s due to an expansion of the atmospheric observation network. The 2 sigma uncertainties in fossil fuel emissions have increased from 0.3 Pg C yr(-1) in the 1960s to almost 1.0 Pg C yr(-1) during the 2000s due to differences in national reporting errors and differences in energy inventories. Lastly, while land use emissions have remained fairly constant, their errors still remain high and thus their global C uptake uncertainty is not trivial. Currently, the absolute errors in fossil fuel emissions rival the total emissions from land use, highlighting the extent to which fossil fuels dominate the global C budget. Because errors in the atmospheric growth rate have decreased faster than errors in total emissions have increased, a similar to 20% reduction in the overall uncertainty of net C global uptake has occurred. Given all the major sources of error in the global C budget that we could identify, we are 93% confident that terrestrial C uptake has increased and 97% confident that ocean C uptake has increased over the last 5 decades. Thus, it is clear that arguably one of the most vital ecosystem services currently provided by the biosphere is the continued removal of approximately half of atmospheric CO2 emissions from the atmosphere, although there are certain environmental costs associated with this service, such as the acidification of ocean waters.
机译:在过去的五十年中,已经开发了监测系统来检测大气和海洋中碳(C)积累的变化;但是,我们检测全局C循环行为变化的能力仍然受到测量和估计误差的阻碍。在这里,我们提出了一个严格而灵活的框架,用于评估估计误差的时空分量及其对生物圈净碳吸收不确定性的影响。我们提出了一种新颖的方法,将时间相关的随机误差纳入排放估算的误差结构中。基于这种方法,我们得出结论,由于大气的膨胀,大气增长率的2 sigma不确定性已从1960年代的1.2 Pg C yr(-1)降低到2000年代的0.3 Pg C yr(-1)。观察网。由于国家报告误差和能源清单的差异,化石燃料排放中的2σ不确定性已从1960年代的0.3 Pg C yr(-1)增加到2000年代的近1.0 Pg C yr(-1)。最后,尽管土地使用排放量保持相当恒定,但其误差仍然很高,因此其全球碳吸收不确定性并非无关紧要。当前,化石燃料排放的绝对误差可与土地利用的总排放量相媲美,这突出了化石燃料在全球碳预算中的主导地位。由于大气增长率的误差下降速度快于总排放量误差的上升速度,因此全球净碳吸收总量的总体不确定性下降了约20%。考虑到我们可以确定的全球C预算中所有主要错误来源,我们有93%的信心对陆地C的吸收有所增加,而97%的人对海洋C的吸收在过去5年中的增长充满信心。因此,很明显,可以说,生物圈目前提供的最重要的生态系统服务之一是继续从大气中清除大约一半的大气CO2排放,尽管与此服务相关的某些环境成本,例如酸化海洋水域。

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