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Global mapping of attenuation at Ku- and Ka-band

机译:Ku和Ka频段衰减的全局映射

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The propagation of radio waves for Earth-space slant path at C-band and higher frequencies is dominated by precipitation in the atmosphere. At a given frequency, attenuation depends on the length of the radio path, the size distribution, and the phase state of the hydrometeor profile. Using the observations from the Tropical Rainfall Measuring Mission (TRMM) spaceborne Ku-band (13.8 GHz) radar at low Earth orbit of 350 km above Earth, global attenuation maps are produced at the Ku-band frequency. A simple microphysical model for precipitation developed using hydrometeor size distributions and thermodynamic phase state is used to estimate attenuation and reflectivity observations at Ka-band (35 GHz) where numerous high-bandwidth satellite applications are being planned including the next-generation space-based radar for the Global Precipitation Mission (GPM). Differences in the microphysical structure in convective and stratiform precipitation are also incorporated in the model. The results show substantial attenuation variation in a 12-month period at both Ku- and Ka-bands over the various regions of the globe, including the contrast between land and ocean. The estimates of attenuation made at Ku- and Ka-band will be useful in the design and development of spaceborne systems.
机译:C波段和更高频率的地球-空间倾斜路径的无线电波传播受大气中降水的支配。在给定的频率下,衰减取决于无线电路径的长度,大小分布以及水凝磁剖面的相态。利用来自热带降雨测量团(TRMM)的星载Ku波段(13.8 GHz)雷达在地球上方350 km的低地球轨道上的观测结果,在Ku波段频率上绘制了全球衰减图。利用水流星大小分布和热力学相态建立的简单的降水微物理模型,用于估算在Ka波段(35 GHz)处的衰减和反射率观测,在该波段中,计划进行众多高带宽卫星应用,包括下一代天基雷达为全球降水任务(GPM)。对流和层状降水的微物理结构差异也纳入了模型。结果表明,在全球各个地区的Ku和Ka波段,在12个月的时间内衰减都有很大变化,包括陆地和海洋之间的对比度。在Ku和Ka波段进行的衰减估计将对空间系统的设计和开发有用。

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