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Comparisons of box model calculations and measurements of formaldehyde from the 1997 North Atlantic Regional Experiment

机译:盒模型计算与1997年北大西洋区域甲醛测量结果的比较

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摘要

Formaldehyde (CH2O) measurements from two independent instruments are compared with photochemical box model calculations. The measurements were made on the National Oceanic and Atmospheric Administration P-3 aircraft as part of the 1997 North Atlantic Regional Experiment (NARE 97). The data set considered here consists of air masses sampled between 0 and 8 km over the North Atlantic Ocean which do not show recent influence from emissions or transport. These air masses therefore should be in photochemical steady state with respect to CH2O when constrained by the other P-3 measurements, and methane oxidation was expected to be the predominant source of CH2O in these air masses. For this data set both instruments measured identical CH2O concentrations to within 40 parts per trillion by volume (pptv) on average over the 0–800 pptv range, although differences larger than the combined 2σ total uncertainty estimates were observed between the two instruments in 11% of the data. Both instruments produced higher CH2O concentrations than the model in more than 90% of this data set, with a median measured-modeled [CH2O] difference of 0.13 or 0.18 ppbv (depending on the instrument), or about a factor of 2. Such large differences cannot be accounted for by varying model input parameters within their respective uncertainty ranges. After examining the possible reasons for the model-measurement discrepancy, we conclude that there are probably one or more additional unknown sources of CH2O in the North Atlantic troposphere.
机译:将两种独立仪器的甲醛(CH2O)测量值与光化学盒模型计算结果进行了比较。作为1997年北大西洋区域实验(NARE 97)的一部分,在美国国家海洋和大气管理局P-3飞机上进行了测量。此处考虑的数据集由北大西洋0-8公里之间采样的空气质量组成,这些空气质量未显示排放或运输的近期影响。因此,当受到其他P-3测量的限制时,这些空气团应相对于CH2O处于光化学稳定状态,并且甲烷氧化被认为是这些空气团中CH2O的主要来源。对于此数据集,两种仪器在0–800 pptv范围内测得的相同CH2O浓度平均在40万亿分之(pptv)范围内,尽管在两种仪器之间观察到的差异大于合并的2σ总不确定性估计值,差异为11%的数据。在此数据集的90%以上中,两种仪器均产生比模型更高的CH2O浓度,实测模型化[CH2O]差异中位数为0.13或0.18 ppbv(取决于仪器),或约为2倍。不能通过在各自不确定性范围内更改模型输入参数来解决差异。在检查了模型测量差异的可能原因后,我们得出结论,北大西洋对流层中可能还有一个或多个其他未知的CH2O来源。

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