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Calculations of Surface Clutter Interference with Precipitation Measurement from Space by 35.5 GHz Radar for Global Precipitation Measurement Mission

机译:用35.5 GHz雷达对全球降水测量任务的空间降水测量的表面杂波干扰

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Surface clutter interference with precipitation measurement from space using 35.5 GHz radar was evaluated for the Global Precipitation Measurement (GPM) Mission. The GPM Mission is unique in that it consists of a core satellite with dual-frequency precipitation radar (13.6 GHz and 35.5 GHz) and eight small companion satellites that are equipped with microwave radiometers. The 35.5 GHz precipitation radar has very high sensitivity; its designed minimum detectable rain rate at the rain top is 0.3 mm/h. In this study, a Taylor distribution with random errors in the excitation current is considered in calculating the radiation pattern of a 35.5 GHz slotted waveguide planar phased array antenna. The signal-to-clutter power ratio (S/C) was evaluated for the antenna pattern given by the Taylor distribution (peak side lobe level = -35dB, n=6; the same values as for the TRMM PR), where S is the received power from the rain scattering volume and C is the backscattered power from sea surface. Uniform rain rates of 0.3 and 1.0 mm/h were assumed in the calculation of S. We show that the interference of surface clutter with precipitation measurement can be suppressed more at 35.5 GHz than at 13.6 GHz because of the short wavelength. The calculated S/C ratio distribution showed that the effect of the side lobe clutter is not negligible, especially for low rain rates (less than 1.0 mm/h), but it is negligible for heavier rain (over 1.0 mm/h). The calculations also show that the effect of the main lobe clutter is severe and not negligible for either light or heavy rain. The conclusion is that 35.5 GHz precipitation radar can accurately observe rain with a planar phased array antenna fed with a Taylor distribution (n=6, peak side lobe level = -35 dB).
机译:从使用35.5 GHz的雷达空间降水测量地面杂波干扰被评价为全球降水测量(GPM)任务。的GPM团是独特的,它由具有双频沉淀雷达(13.6 GHz和35.5千兆赫)和配备有微波辐射计八个小伴侣卫星芯卫星的。在35.5 GHz的沉淀雷达具有非常高的灵敏度;在雨顶部其设计最小可检测降雨速率为0.3毫米/小时。在这项研究中,在励磁电流与随机误差的泰勒分布在计算35.5 GHz的缝隙波导的平面相控阵天线的辐射图案被考虑。信号杂波功率比(S / C)评价由泰勒分布给出的天线图案(峰值旁瓣电平= -35dB,N = 6;相同的值作为用于TRMM PR),其中S是从雨散射体积和C的接收功率是从海面反向散射功率。的0.3和1.0毫米/小时均匀降雨率假定是在S的计算我们表明,表面的杂波与降水测量的干扰可以更在35.5 GHz的在13.6 GHz的,因为短波长的抑制比。计算出的S / C比的分布表明,该旁瓣杂波的影响是不可忽略的,尤其是对于低降雨率(小于1.0毫米/小时),但它是可以忽略对于较重雨(超过1.0毫米/小时)。计算还表明,主瓣杂波的影响是严重的,不可忽略的光或大暴雨。结论是35.5 GHz的沉淀雷达能够准确地观察雨与平面相控用泰勒分布馈送阵列天线(N = 6,峰旁瓣电平= -35分贝)。

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