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首页> 外文期刊>Boundary-layer Meteorology >A Wavelet-Based Correction Method for Eddy-Covariance High-Frequency Losses in Scalar Concentration Measurements
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A Wavelet-Based Correction Method for Eddy-Covariance High-Frequency Losses in Scalar Concentration Measurements

机译:标量浓度测量中涡流协方差高频损耗的小波校正方法

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Eddy-covariance (EC) scalar-ux measurements suffer from unavoidable biases introduced by high-frequency losses in the sampled scalar concentration uctuations. This bias alone leads to an underestimation of scalar uxes by as much as 20% in some cases, especially when a closed-path gas analyzer is used to sample concentration far from the inlet location. A novel method that directly corrects for these high-frequency losses using only the sampled scalar-concentration time series is proposed and tested. The sampled concentration uctuation time series is adjusted, point-by-point, in the wavelet half-plane for each EC averaging interval (≈30 min). Similarity between scalars (and temperature) is not necessary and a pre-dened theoretical shape of the cospectrum is not required, making this method attractive at meteorologically non-ideal sites. When closed-path gas analyzers are used to measure H2O concentration uctuations, the method is shown to reproduce the dependence of the attenuation on air relative humidity. Nevertheless, the method is not able to account for excessively large spectral attenuation that occurs close to the spectral peak, as might be the case with long tubes and high relative humidity. Since the method corrects the original scalar concentration time series and not the cospectrum, other ow statistics—such as variances and integral time scales—are also adjusted. The proposed method can be used synergistically with conventional high-frequency cospectral correction methods given the differences in assumptions and approaches among these methods. When the conventional and the proposed methods agree, added condence to the estimate of the high frequency correction is gained, and vice versa.
机译:涡度协方差(EC)标量ux测量的结果是不可避免的偏差是由采样标量浓度曲线中的高频损耗引起的。在某些情况下,尤其是当使用闭路气体分析仪对远离进口位置的浓度进行采样时,仅凭这种偏见会导致标量量低估多达20%。提出并测试了一种仅使用采样的标量集中时间序列直接校正这些高频损耗的新颖方法。对于每个EC平均间隔(约30分钟),在小波半平面中逐点调整采样浓度变化时间序列。标量(和温度)之间的相似性不是必需的,并且副谱的预先确定的理论形状也不是必需的,这使该方法在气象学上非理想的位置具有吸引力。当使用闭路气体分析仪测量H2O浓度变化时,该方法显示出可再现衰减对空气相对湿度的依赖性。然而,该方法不能解决在靠近光谱峰值处发生的过大光谱衰减的问题,长管和高相对湿度的情况可能如此。由于该方法校正的是原始标量浓度时间序列,而不是协谱,因此还调整了其他流量统计数据,例如方差和积分时间标度。假设这些方法之间的假设和方法不同,则可以与常规的高频共谱校正方法协同使用。当常规方法和提出的方法相吻合时,就可以增加高频校正估计的可信度,反之亦然。

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