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A Method for Estimating the Turbulent Kinetic Energy Dissipation Rate from a Vertically Pointing Doppler Lidar, and Independent Evaluation from Balloon-Borne In Situ Measurements

机译:一种从垂直指向多普勒激光雷达估计湍流动能耗散率的方法,以及气球原位测量的独立评估

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摘要

A method of estimating dissipation rates from a vertically pointing Doppler lidar with high temporal and spatial resolution has been evaluated by comparison with independent measurements derived from a balloon-borne sonic anemometer. This method utilizes the variance of the mean Doppler velocity from a number of sequential samples and requires an estimate of the horizontal wind speed. The noise contribution to the variance can be estimated from the observed signal-to-noise ratio and removed where appropriate. The relative size of the noise variance to the observed variance provides a measure of the confidence in the retrieval. Comparison with in situ dissipation rates derived from the balloon-borne sonic anemometer reveal that this particular Doppler lidar is capable of retrieving dissipation rates over a range of at least three orders of magnitude. This method is most suitable for retrieval of dissipation rates within the convective well-mixed boundary layer where the scales of motion that the Doppler lidar probes remain well within the inertial subrange. Caution must be applied when estimating dissipation rates in more quiescent conditions. For the particular Doppler lidar described here, the selection of suitably short integration times will permit this method to be applicable in such situations but at the expense of accuracy in the Doppler velocity estimates. The two case studies presented here suggest that, with profiles every 4 s, reliable estimates of ε can be derived to within at least an order of magnitude throughout almost all of the lowest 2 kmand, in the convective boundary layer, to within 50%. Increasing the integration time for individual profiles to 30 s can improve the accuracy substantially but potentially confines retrievals to within the convective boundary layer. Therefore, optimization of certain instrument parameters may be required for specific implementations.
机译:通过与气球声波风速计得出的独立测量结果进行比较,已评估了一种估算具有高时空分辨率的垂直指向多普勒激光雷达耗散率的方法。该方法利用了来自多个连续样本的平均多普勒速度的方差,并需要估计水平风速。可以根据观察到的信噪比估算噪声对方差的贡献,并在适当的地方将其消除。噪声方差与观察到的方差的相对大小提供了对检索的置信度的度量。与气球式声速计得出的原位耗散率的比较表明,这种特定的多普勒激光雷达能够在至少三个数量级的范围内获取耗散率。该方法最适合于对流良好混合边界层内的耗散率的恢复,在该边界层中多普勒激光雷达探测器的运动尺度很好地保持在惯性子范围内。在更静态的情况下估计耗散率时必须谨慎。对于此处描述的特定多普勒激光雷达,选择合适的短积分时间将使该方法适用于此类情况,但会牺牲多普勒速度估算的准确性。这里介绍的两个案例研究表明,每隔4 s就有一次剖面,ε的可靠估计值可以在对流边界层中几乎所有最低的2 km范围内至少在一个数量级内得出,并且在50%以内。将单个剖面的积分时间增加到30 s可以显着提高精度,但有可能将检索范围限制在对流边界层内。因此,对于特定的实现,可能需要优化某些仪器参数。

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