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Dual-Doppler and Polarimetric Radar Analysis of Hail Events in Germany

机译:德国冰雹事件的双多普勒和极化雷达分析

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Understanding the life cycle of precipitating systems is important for better nowcasting of significant weather and for improving weather prediction models. Doppler and polarimetric weather radars have the ability to look simultaneously into the microphysics and dynamics of precipitation systems. In this work we make use of these powerful tools to perform a combined analysis of the dynamics and microphysics of precipitation systems, in order to better understand storm development. By using data from multiple Doppler radars, the 3D wind field may be retrieved. Simultaneously, the polarimetric capability of the radars allows the retrieval of hydrometeor types and microphysical processes. Therefore, we are able to identify the processes through which precipitation systems evolve by revealing the interdependence between storm dynamics and microphysics. Prominent examples of such interactions are the development of socalled Zdr columns, that are associated with storm updrafts, and consequent freezing and potential hail formation; or regions of riming that are difficult to spot from polarimetry alone, but which require an updraft for supply of supercooled water, which could be seen in the wind field retrievals; or the development of lightning through lifting of graupel in convective updrafts that cause vertical electric charge separation. In this work we apply the Dual-Doppler technique DDA to analyze two large hail events that occurred near the Bonn and Jülich radars: the 5thJuly 2015 and 22 June 2017. The life cycle of these 2 systems will be examined to better understand the formation and growth of hail, from the perspective of dynamics and microphysics.
机译:了解降水系统的生命周期对于更好地预报重要天气和改善天气预报模型非常重要。多普勒和极化气象雷达具有同时观察降水系统的微物理学和动力学的能力。在这项工作中,我们利用这些强大的工具对降水系统的动力学和微观物理学进行综合分析,以便更好地了解风暴的发展。通过使用来自多个多普勒雷达的数据,可以检索3D风场。同时,雷达的极化能力允许检索水凝物类型和微物理过程。因此,通过揭示风暴动力学与微观物理学之间的相互依存关系,我们能够确定降水系统演化的过程。这种相互作用的突出例子是发展了所谓的Zdr柱,这些柱与暴风雨上升,随之而来的冰冻和潜在的冰雹形成有关。或仅通过极化法难以发现的边缘区域,但需要向上流动以供应过冷水,这可以在风场检索中看到;或通过对流上升气流中的格栅提升产生雷电,导致垂直电荷分离。在这项工作中,我们应用双多普勒技术DDA分析波恩和尤利希雷达附近发生的两个大雹事件:第5个 2015年7月和2017年6月22日。将从动力学和微观物理学的角度检查这两个系统的生命周期,以更好地了解冰雹的形成和增长。

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