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Antarctic Surface Reflectivity Measurements from the ANITA-3 and HiCal-1 Experiments

机译:来自ANITA-3和HiCal-1实验的南极表面反射率测量

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The primary science goal of the NASA-sponsored ANITA project is measurement of ultra-high energy neutrinos and cosmic rays, observed via radio-frequency signals resulting from a neutrino or cosmic ray interaction with terrestrial matter (e.g. atmospheric or ice molecules). Accurate inference of the energies of these cosmic rays requires understanding the transmission/reflection of radio wave signals across the ice–air boundary. Satellite-based measurements of Antarctic surface reflectivity, using a co-located transmitter and receiver, have been performed more-or-less continuously for the last few decades. Our comparison of four different reflectivity surveys, at frequencies ranging from 2 to 45GHz and at near-normal incidence, yield generally consistent maps of high versus low reflectivity, as a function of location, across Antarctica. Using the Sun as an RF source, and the ANITA-3 balloon borne radio-frequency antenna array as the RF receiver, we have also measured the surface reflectivity over the inter...
机译:由NASA赞助的ANITA项目的主要科学目标是测量超高能中微子和宇宙射线,通过中微子或宇宙射线与地面物质(例如大气或冰分子)相互作用产生的射频信号进行观测。准确推断这些宇宙射线的能量需要了解跨冰冰边界的无线电波信号的传输/反射。在过去的几十年中,使用发射器和接收器位于同一地点,对南极表面反射率进行了基于卫星的测量。我们对频率范围从2到45GHz且接近法线入射的四个不同反射率调查的比较,得出了整个南极洲的高反射率和低反射率的大致一致的图,这些图是位置的函数。使用太阳作为射频源,并使用ANITA-3气球式射频天线阵列作为射频接收器,我们还测量了整个传感器之间的表面反射率。

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