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首页> 外文期刊>Atmospheric Measurement Techniques >Correcting atmospheric COsub2/sub and CHsub4/sub mole fractions obtained with Picarro analyzers for sensitivity of cavity pressure to water vapor
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Correcting atmospheric COsub2/sub and CHsub4/sub mole fractions obtained with Picarro analyzers for sensitivity of cavity pressure to water vapor

机译:校正使用Picarro分析仪获得的大气CO 2 和CH 4 摩尔分数以提高空腔压力对水蒸气的敏感性

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Measurements of dry air mole fractions of atmospheric greenhouse gases are used in inverse models of atmospheric tracer transport to quantify their sources and sinks. The measurements have to be calibrated to a common scale to avoid bias in the inferred fluxes. For this purpose, the World Meteorological Organization (WMO) has set requirements for the interlaboratory compatibility of atmospheric greenhouse gas (GHG) measurements. A widely used series of devices for these measurements are the GHG analyzers manufactured by Picarro, Inc. These are often operated in humid air, and the effects of water vapor are corrected for in post-processing. Here, we report on rarely detected and previously unexplained biases of the water correction method for COsub2/sub and CHsub4/sub in the literature. They are largest at water vapor mole fractions below 0.5?% Hsub2/subO , which were undersampled in previous studies, and can therefore affect measurements obtained in humid air. Setups that dry sample air using Nafion membranes may be affected as well if there are differences in residual water vapor levels between sample and calibration air. The biases are caused by a sensitivity of the pressure in the measurement cavity to water vapor. We correct these biases by modifying the water correction method from the literature. Our method relies on experiments that maintain stable water vapor levels to allow equilibration of cavity pressure. In our experiments with the commonly used droplet method, this requirement was not fulfilled. Correcting COsub2/sub measurements proved challenging, presumably because of our humidification method. Open questions pertain to differences among analyzers and variability over time. In our experiments, the biases amounted to considerable fractions of the WMO interlaboratory compatibility goals. Since measurements of dry air mole fractions of COsub2/sub and CHsub4/sub are also subject to other uncertainties, correcting the cavity pressure-related biases helps keep the overall accuracy of measurements obtained with Picarro GHG analyzers in humid and potentially in Nafion-dried air within the WMO goals.
机译:大气示踪剂迁移的反模型中使用了大气温室气体的干燥空气摩尔分数的测量值,以量化其源和汇。必须将测量值校准到通用比例,以避免推断出的通量出现偏差。为此,世界气象组织(WMO)为大气温室气体(GHG)测量的实验室间兼容性设定了要求。 Picarro,Inc.制造的GHG分析仪是用于这些测量的一系列广泛使用的设备。它们通常在潮湿的空气中运行,并且在后处理中校正了水蒸气的影响。在这里,我们报道了文献中针对CO 2 和CH 4 的水校正方法很少发现和无法解释的偏差。在低于0.5?%H 2 O的水蒸气摩尔分数处,它们最大,而在先前的研究中采样不足,因此会影响在潮湿空气中获得的测量结果。如果样品空气和校准空气之间残留的水蒸气含量存在差异,使用Nafion膜干燥样品空气的设置也会受到影响。偏差是由测量腔中的压力对水蒸气的敏感性引起的。我们通过修改文献中的水校正方法来校正这些偏差。我们的方法依赖于维持稳定水蒸气水平以平衡型腔压力的实验。在我们使用常用的液滴法进行的实验中,未满足此要求。事实证明,校正CO 2 测量值具有挑战性,这可能是因为我们采用了加湿方法。悬而未决的问题涉及分析仪之间的差异以及随着时间的变化。在我们的实验中,偏差占WMO实验室间兼容性目标的相当一部分。由于CO 2 和CH 4 的干燥空气摩尔分数的测量也受到其他不确定性的影响,校正与腔压力有关的偏差有助于保持通过在WMO目标范围内,Picarro GHG分析仪可以在潮湿的地方,也可以在Nafion干燥的空气中。

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