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首页> 外文期刊>Atmospheric Measurement Techniques >Eddy-covariance data with low signal-to-noise ratio: time-lag determination, uncertainties and limit of detection
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Eddy-covariance data with low signal-to-noise ratio: time-lag determination, uncertainties and limit of detection

机译:辐射信噪比低的涡流数据:时间滞后确定,不确定性和检测极限

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摘要

All eddy-covariance flux measurements are associated with random uncertainties which are a combination of sampling error due to natural variability in turbulence and sensor noise. The former is the principal error for systems where the signal-to-noise ratio of the analyser is high, as is usually the case when measuring fluxes of heat, CO2 or H2O. Where signal is limited, which is often the case for measurements of other trace gases and aerosols, instrument uncertainties dominate. Here, we are applying a consistent approach based on auto- and cross-covariance functions to quantify the total random flux error and the random error due to instrument noise separately. As with previous approaches, the random error quantification assumes that the time lag between wind and concentration measurement is known. However, if combined with commonly used automated methods that identify the individual time lag by looking for the maximum in the cross-covariance function of the two entities, analyser noise additionally leads to a systematic bias in the fluxes. Combining data sets from several analysers and using simulations, we show that the method of time-lag determination becomes increasingly important as the magnitude of the instrument error approaches that of the sampling error. The flux bias can be particularly significant for disjunct data, whereas using a prescribed time lag eliminates these effects (provided the time lag does not fluctuate unduly over time). We also demonstrate that when sampling at higher elevations, where low frequency turbulence dominates and co-variance peaks are broader, both the probability and magnitude of bias are magnified. We show that the statistical significance of noisy flux data can be increased (limit of detection can be decreased) by appropriate averaging of individual fluxes, but only if systematic biases are avoided by using a prescribed time lag. Finally, we make recommendations for the analysis and reporting of data with low signal-to-noise and their associated errors.
机译:所有EDDY-Covariance磁通量测量与随机不确定性相关联,这是由于湍流和传感器噪声的自然可变性而采样误差的组合。前者是分析仪的信噪比高的系统的主要误差,通常情况下测量热量,二氧化碳或H2O的助熔剂时。当信号有限的地方,这通常是用于测量其他痕量气体和气溶胶的情况,仪器不确定性占主导地位。在这里,我们正在基于自动和交叉协方差函数应用一致的方法来量化由于仪器噪声分别而导致的总随机磁通误差和随机误差。与以前的方法一样,随机误差量化假定风和浓度测量之间的时间滞后是已知的。然而,如果通过寻找两个实体的交叉协方差函数中的最大值来结合识别各个时间滞后的常用自动化方法,则分析器噪声另外导致通量的系统偏差。组合数据集从多个分析仪和使用模拟,我们表明,随着仪器误差的幅度接近采样误差的时间,时间滞后确定的方法变得越来越重要。磁通偏压对于分离数据可能特别显着,而使用规定的时间滞后消除了这些效果(如果时间滞后不会过度波动)。我们还证明,当在更高的高度处抽样时,在低频湍流主导和共方峰值更宽的情况下,偏置的概率和大小都被放大。我们表明,可以通过适当平均各个助熔剂的适当平均来增加噪声磁通数据的统计显着性(可以减少检测限),而是仅通过使用规定的时间滞后避免系统偏差。最后,我们提出了对具有低信噪比及其相关错误的数据的分析和报告的建议。

著录项

  • 来源
    《Atmospheric Measurement Techniques》 |2015年第10期|共17页
  • 作者单位

    Ctr Ecol &

    Hydrol Penicuik EH26 0QB Midlothian Scotland;

    Univ Lancaster Lancaster Environm Ctr Lancaster LA1 4YQ England;

    Climate &

    Air Pollut Grp Agroscope Res Stn Zurich Switzerland;

    Univ Lancaster Lancaster Environm Ctr Lancaster LA1 4YQ England;

    Ctr Ecol &

    Hydrol Penicuik EH26 0QB Midlothian Scotland;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 计量学;
  • 关键词

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