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On the potential of sub-mm passive MW observations from geostationary satellites to retrieve heavy precipitation over the Mediterranean Area

机译:关于对地静止卫星亚毫米无源兆瓦观测值恢复地中海地区强降水的潜力

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摘要

The general interest in the potential use of the mm and sub-mm frequenciesup to 425 GHz resolution from geostationary orbit is increasing due to thefact that the frequent time sampling and the comparable spatial resolutionrelative to the "classical" (≤89 GHz) microwave frequencies wouldallow the monitoring of precipitating intense events for the assimilation ofrain in now-casting weather prediction models.In this paper, we use the simulation of a heavy precipitating event in frontof the coast of Crete island (Greece) performed by the University ofWisconsin - Non-hydrostatic Modeling System (UW-NMS) cloud resolving modelin conjunction with a 3D-adjusted plane parallel radiative transfer model tosimulate the upwelling brightness temperatures (TB's) at mm and sub-mmfrequencies. To study the potential use of high frequencies, we firstanalyze the relationships of the simulated TB's with the microphysicalproperties of the UW-NMS simulated precipitating clouds, and then explorethe capability of a Bayesian algorithm for the retrieval of surface rainrate, rain and ice water paths at such frequencies.
机译:对地球静止轨道最高达425 GHz分辨率的毫米和亚毫米频率的潜在用途的普遍关注正在增加,原因是事实是频繁的时间采样和相对于“经典”(≤89GHz)微波频率的可比空间分辨率在现在预报的天气预报模型中,对强降水事件的监测以吸收雨水。 本文中,我们使用了由克里特岛(希腊)海岸前部进行的一次强降水事件的模拟。威斯康星大学-非静水模型系统(UW-NMS)云解析模型与3D调整后的平面平行辐射传输模型相结合,可模拟毫米和亚毫米频率处的上升流亮度温度(TB)。为了研究高频的潜在用途,我们首先分析模拟结核与UW-NMS模拟降水云的微观物理特性之间的关系,然后探索贝叶斯算法在地面降水,雨水和冰水路径上的反演能力。这样的频率。

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