首页> 外文期刊>Atmospheric Chemistry and Physics Discussions >Estimation of continuous anthropogenic COsub2/sub: model-based evaluation of COsub2/sub, CO, ?′sup13/supC(COsub2/sub) and ??sup14/supC(COsub2/sub) tracer methods
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Estimation of continuous anthropogenic COsub2/sub: model-based evaluation of COsub2/sub, CO, ?′sup13/supC(COsub2/sub) and ??sup14/supC(COsub2/sub) tracer methods

机译:连续人为产生的CO 2 的估计:基于模型的CO 2 ,CO,α' 13 C(CO 2 )和?? 14 C(CO 2 )跟踪器方法

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pstrongAbstract./strong We investigate different methods for estimating anthropogenic COsub2/sub using modeled continuous atmospheric concentrations of COsub2/sub alone, as well as COsub2/sub in combination with the surrogate tracers CO, δsup13/supC(COsub2/sub) and ??sup14/supC(COsub2/sub). These methods are applied at three hypothetical stations representing rural, urban and polluted conditions. We find that, independent of the tracer used, an observation-based estimate of continuous anthropogenic COsub2/sub is not yet feasible at rural measurement sites due to the low signal-to-noise ratio of anthropogenic COsub2/sub estimates at such settings. The tracers δsup13/supC(COsub2/sub) and CO provide an accurate possibility to determine anthropogenic COsub2/sub continuously, only if all COsub2/sub sources in the catchment area are well characterized or calibrated with respect to their isotopic signature and CO to anthropogenic COsub2/sub ratio. We test different calibration strategies for the mean isotopic signature and CO to COsub2/sub ratio using precise ??sup14/supC(COsub2/sub) measurements on monthly integrated as well as on grab samples. For δsup13/supC(COsub2/sub), a calibration with annually averaged sup14/supC(COsub2/sub) grab samples is most promising, since integrated sampling introduces large biases into anthropogenic COsub2/sub estimates. For CO, these biases are smaller. The precision of continuous anthropogenic COsub2/sub determination using ?′sup13/supC(COsub2/sub) depends on measurement precision of ?′sup13/supC(COsub2/sub) and COsub2/sub, while the CO method is mainly limited by the variation in natural CO sources and sinks. At present, continuous anthropogenic COsub2/sub could be determined using the tracers ?′sup13/supC(COsub2/sub) and/or CO with a precision of about 30 %, a mean bias of about 10 % and without significant diurnal discrepancies. Hypothetical future measurements of continuous ??sup14/supC(COsub2/sub) with a precision of 5 ‰ are promising for anthropogenic COsub2/sub determination (precision ca. 10a??20 %) but are not yet available. The investigated tracer-based approaches open the door to improving, validating and reducing biases of highly resolved emission inventories using atmospheric observation and regional modeling./p.
机译:> >摘要。我们研究了单独使用模拟的CO 2 和CO 的连续大气浓度来估算人为CO 2 的不同方法。 sub> 2 与替代示踪剂CO,δ 13 C(CO 2 )和?? 14 C( CO 2 )。这些方法应用于代表农村,城市和污染状况的三个假设站点。我们发现,不管使用哪种示踪剂,由于人为产生的CO 2 的信噪比低,在农村测量点对人为的连续CO 2 进行基于观测的估计尚不可行。在这种设置下> 2 估算。示踪剂&ltta; 13 C(CO 2 )和CO提供了连续确定人为源CO 2 的准确可能性,除非所有CO 2 的同位素特征,CO与人为的CO 2 的比例方面,已经得到了很好的表征或校准。我们每月使用精确的?? 14 C(CO 2 )测量来测试平均同位素特征和CO与CO 2 比的不同校准策略集成样本以及样品样本。对于δ 13 C(CO 2 ),使用年均 14 C(CO 2 )抓取进行校准样本是最有前途的,因为综合抽样将人为的CO 2 估计值引入较大的偏差。对于CO,这些偏差较小。使用?′ 13 C(CO 2 )连续人为确定CO 2 的精度取决于?′ 13 < / sup> C(CO 2 )和CO 2 ,而CO方法主要受天然CO源和汇变化的限制。目前,可以使用示踪剂?' 13 C(CO 2 )和/或CO来确定连续的人为CO 2 和CO,精度为大约30%,平均偏差大约10%,并且没有明显的昼夜差异。连续?? 14 C(CO 2 )的假想未来测量,精度为5&permil;有望用于人为的CO 2 测定(精确度约为10a ?? 20%),但尚无可用。研究的基于示踪剂的方法为利用大气观测和区域模型改善,验证和减少高分辨排放清单的偏差打开了大门。

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