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Optimal estimation of water vapour profiles using a combination of Raman lidar and microwave radiometer

机译:拉曼激光雷达和微波辐射计相结合的最佳水汽剖面估算

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摘要

In this work, a two-step algorithm to obtain water vapour profiles froma combination of Raman lidar and microwave radiometer is presented. Bothinstruments were applied during an intensive 2-month measurement campaign(HOPE) close to Jülich, western Germany, during spring 2013. To retrievereliable water vapour information from inside or above the cloud a two-stepalgorithm is applied. The first step is a Kalman filter that extends theprofiles, truncated at cloud base, to the full height range (up to 10 km) bycombining previous information and current measurement. Then the completewater vapour profile serves as input to the one-dimensional variational(1D-VAR) method, also known as optimal estimation. A forward model simulatesthe brightness temperatures which would be observed by the microwaveradiometer for the given atmospheric state. The profile is iterativelymodified according to its error bars until the modelled and the actuallymeasured brightness temperatures sufficiently agree. The functionality of theretrieval is presented in detail by means of case studies under differentconditions. A statistical analysis shows that the availability of Raman lidardata (night) improves the accuracy of the profiles even under cloudyconditions. During the day, the absence of lidar data results in largerdifferences in comparison to reference radiosondes. The data availability ofthe full-height water vapour lidar profiles of 17 % during the 2-monthcampaign is significantly enhanced to 60 % by applying the retrieval. Thebias with respect to radiosonde and the retrieved a posteriori uncertainty ofthe retrieved profiles clearly show that the application of the Kalman filterconsiderably improves the accuracy and quality of the retrieved mixing ratioprofiles.
机译:在这项工作中,提出了一种通过拉曼激光雷达和微波辐射计的组合获得水蒸气剖面的两步算法。在2013年春季期间,这两个仪器均在德国西部尤利希附近进行了为期2个月的密集测量活动(HOPE)中使用。为了从云内部或上方检索可靠的水蒸气信息,使用了两步算法。第一步是卡尔曼滤波器,通过结合先前的信息和当前的测量值,将在云底截断的轮廓扩展到整个高度范围(最大10千米)。然后,完整的水蒸气剖面将用作一维变分(1D-VAR)方法的输入,该方法也称为最佳估计。一个正向模型模拟了在给定的大气状态下微波辐射计会观测到的亮度温度。根据其误差线对轮廓进行迭代修改,直到建模和实际测量的亮度温度完全一致为止。在不同条件下,通过案例研究详细介绍了检索功能。统计分析表明,即使在多云条件下,拉曼激光雷达数据(夜间)的可用性也提高了剖面的准确性。与参考无线电探空仪相比,白天没有激光雷达数据会导致更大的差异。通过应用检索,在两个月的运动中全高水汽激光雷达剖面的数据可用性为17%,大大提高了60%。相对于探空仪的偏见和所取回剖面的后验不确定性清楚地表明,卡尔曼滤波器的应用极大地提高了所取回混合比剖面的准确性和质量。

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