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Refined Physical Retrieval of Integrated Water Vapor and Cloud Liquid for Microwave Radiometer Data

机译:完善的水蒸气和云层液体综合物理检索,用于微波辐射计数据

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Monitoring atmospheric water is essential for the understanding of the dynamic processes of the atmosphere and for the assessment of wave-propagation properties. Microwave radiometers, in combination with a thermal infrared channel, have the potential to fulfill these tasks. This paper is focused on the surface-based system TROWARA with microwave channels at 21.3 and 31.5 GHz. TROWARA has been used for tropospheric water measurements at Bern since 1994 together with a standard meteo station. So far, emphasis has been put on integrated water vapor (IWV) measurements, particularly for climate studies, but integrated liquid water (ILW) has been retrieved as well. We report on methodological advances with the data analysis. First, the original algorithm was replaced by a new statistical retrieval based on the simulations of TROWARA data using radiosonde profiles. Second, in a physical refinement, the cause of the variable ILW bias has been identified, and a method for its reduction to the level of 0.001 to 0.005 mm has been developed and tested. The bias is mainly a result of the variable water-vapor influence on absorption at 31 GHz. The bias correction also influences the IWV retrieval. The refined physical retrieval includes the temperature dependence of cloud absorption based on a recent dielectric model of water. The three algorithms (original, new, and refined) have been compared for two years of data. The applications of the refined algorithm are focused on physical processes, such as the development of supercooled clouds. Future advances will include precipitation measurements.
机译:监测大气水对于理解大气的动态过程和评估波的传播特性至关重要。微波辐射计与热红外通道相结合,有潜力完成这些任务。本文的重点是具有微波通道21.3和31.5 GHz的基于表面的系统TROWARA。自1994年以来,TROWARA与标准的气象站一起已在伯尔尼用于对流层水的测量。到目前为止,重点已经放在综合水蒸气(IWV)的测量上,尤其是在气候研究中,但是也已经获得了综合液态水(ILW)。我们通过数据分析报告了方法学的进步。首先,原始算法被新的统计检索所取代,该统计检索基于使用探空仪剖面图对TROWARA数据的模拟。第二,在物理上的改进中,已经确定了引起ILW偏差的原因,并且已经开发并测试了将其减小到0.001至0.005 mm的水平的方法。偏差主要是由于水汽变化对31 GHz吸收的影响所致。偏差校正还会影响IWV检索。改进的物理取回包括基于最新的水介电模型的云吸收的温度依赖性。这三种算法(原始算法,新算法和改进算法)已经比较了两年的数据。改进算法的应用集中在物理过程上,例如过冷云的发展。未来的发展将包括降水测量。

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