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ACCOUNTING TECHNOLOGY BY A COUNCIL ON COMPLEMENTARY EVALUATION

机译:理事会关于补充评估的会计技术

摘要

The dimensional distribution of raindrops (N0 asterisk ) is deduced directly from the differential phase difference between r0 and r1 and from integral of the apparent reflectivity Ze, raised to a chosen exponent. The exponent chosen (b) is one which verifies KDP / N0 asterisk = a(Ze / N0 asterisk )b; KDP is the rate of variation of the phase differential along a ray, a and b are specified by the type of precipitation considered and temperature. Method of estimating precipitation rate for rain only generating negligible attenuation, using bipolar radar. Has the following stages: (a) radar measure over a given interval (r0, r1) for a ray trajectory, the differential phase (=FDP) and the apparent reflectivity (Ze) along at least one of the polarizations (H or V); estimate the value (N0), representative of the raindrop dimensional distribution, from the phase difference between r0 and r1 and from an integral of a function of the apparent reflectivity (Ze) along the interval (r0, r1); deduce the value for the precipitation rate at a point from N0 asterisk and the apparent reflectivity at this point. An Independent claim is also included for a precipitation estimating device.
机译:雨滴的尺寸分布(N0星号)直接从r0和r1之间的微分相位差以及视在反射率Ze的积分中推导得出,并升至选定的指数。选择的指数(b)是一个验证KDP / N0星号= a(Ze / N0星号)b的指数; KDP是相差沿射线的变化率,a和b由所考虑的降水类型和温度确定。使用双极雷达估算仅产生可忽略的衰减的降雨的降水率的方法。具有以下阶段:(a)雷达在给定间隔(r0,r1)上测量至少一条偏振方向(H或V)的射线轨迹,微分相位( = FDP)和视在反射率(Ze) );根据r0和r1之间的相位差以及沿间隔(r0,r1)的视在反射率(Ze)的函数的积分,估算代表雨滴尺寸分布的值(N0);从N0星号推导出某个点的降水速率值,并从该点推导出表观反射率。降水量估算设备也包含独立权利要求。

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