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Separation of biospheric and fossil fuel fluxes of CO2 by atmospheric inversion of CO2 and 14CO2 measurements: Observation System Simulations

机译:通过大气CO2反演和14CO2测量分离生物圈和化石燃料通量的二氧化碳:观测系统模拟

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摘要

National annual total CO emissions from combustion of fossil fuelsare likely known to within 5–10 % for most developed countries. However,uncertainties are inevitably larger (by unknown amounts) for emissionestimates at regional and monthly scales, or for developing countries. Givenrecent international efforts to establish emission reduction targets,independent determination and verification of regional and national scalefossil fuel CO emissions are likely to become increasinglyimportant. Here, we take advantage of the fact that precise measurements ofC in CO provide a largely unbiased tracer for recentlyadded fossil-fuel-derived CO in the atmosphere and present anatmospheric inversion technique to jointly assimilate observations ofCO and CO in order to simultaneously estimate fossil fuel emissions and biospheric exchange fluxes of CO. Using this method in a set of Observation System Simulation Experiments (OSSEs), we show that given the coverage of CO measurements available in 2010(969 over North America, 1063 globally), we can recover the US national totalfossil fuel emission to better than 1 % for the year and to within5 % for most months. Increasing the number of COobservations to  ∼ 5000 per year over North America, as recentlyrecommended by the National Academy of Science (NAS) (Pacala et al., 2010), we recover monthly emissions to within 5 % for all months for the US as awhole and also for smaller, highly emissive regions over which the specifieddata coverage is relatively dense, such as for the New England states or theNY-NJ-PA tri-state area. This result suggests that, given continuedimprovement in state-of-the art transport models, a measurement programsimilar in scale to that recommended by the NAS can provide for independentverification of bottom-up inventories of fossil fuel CO at theregional and national scale. In addition, we show that the dual tracerinversion framework can detect and minimize biases in estimates of thebiospheric flux that would otherwise arise in a traditional CO-onlyinversion when prescribing fixed but inaccurate fossil fuel fluxes.
机译:在大多数发达国家中,化石燃料燃烧产生的国家年度二氧化碳总排放量可能在5-10%之内。但是,对于区域和月度尺度的排放估算,或者对于发展中国家,不确定性不可避免地会更大(不确定数量)。鉴于国际上为确定减排目标所做的努力,区域和国家规模化石燃料CO排放量的独立确定和验证可能变得越来越重要。在这里,我们利用以下事实:对CO中C的精确测量为大气中最近添加的化石燃料衍生的CO提供了基本无偏差的示踪剂,并提出了一种大气反演技术以共同吸收CO和CO的观测值,以便同时估算化石燃料的排放量以及在一组观测系统模拟实验(OSSE)中使用这种方法,我们表明,鉴于2010年可用的CO测量范围(北美为969个,全球为1063个),我们可以恢复美国全年的总化石燃料排放量优于1%,而大多数月份则不超过5%。根据美国国家科学院(NAS)最近的建议(北美地区,Pacala等,2010),北美地区每年的CO观测数量增加到5000,我们将美国整个月的月排放量恢复到5%以内。以及指定数据覆盖范围相对密集的较小的高发射区域,例如新英格兰州或NY-NJ-PA三州区域。该结果表明,随着先进运输模型的不断改进,规模与NAS建议的测量程序相似的测量程序可以独立验证区域和国家范围内化石燃料CO自下而上的库存量。此外,我们表明,双重示踪转化框架可以在规定固定但不准确的化石燃料通量时,检测和最小化生物圈通量估算中的偏差,否则这些偏差会在传统的仅CO转化中产生。

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