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Estimates of the integral method for improving humidity of the atmosphere above the ocean on measurements of satellite microwave radiometers

机译:卫星微波辐射计测量提高海洋上方大气湿度的整体方法的估算

摘要

Method improved estimate integral humidity atmosphere over the ocean by measurement of satellite microwave radiometers by obtaining brightness temperature values ​​(T) of the radiometric channels and compute the value of the integral humidity (Q) using the function taking into account the value of the brightness temperature (T) and coefficients configured neural network, numeral values ​​which were obtained by mathematical modeling of the outgoing radiation ocean-atmosphere system and conducting numerical experiments by using neural networks as the operator of solving the inverse problem with the subsequent adjustment process on aligned in space and time of satellite and terrestrial measurements, and wherein the used radiometric five channels that are frequency υ1 = 10.65 GHz, υ2 = 18 7 GHz, υ5 = 36,5 GHz horizontal polarization and υ3,4 = 23,8 GHz vertical and horizontal polarizations, a setting process is performed on the global satellite and terrestrial measurements, which allows to obtain a higher, in comparison with existing , Reconstruction accuracy integral humidity Q over the oceans in all geographical areas in an extended range of ocean and the atmosphere.
机译:通过获取辐射测量通道的亮度温度值(T)并使用考虑了温度值的函数计算积分湿度(Q)的方法,通过测量卫星微波辐射计来改进估算海洋整体湿度的方法亮度温度(T)和系数配置的神经网络,数值是通过对辐射海洋-大气系统的数学建模并通过使用神经网络作为求解器来解决反问题并随后进行调整过程而进行的数值实验而获得的卫星和地面测量的空间和时间对齐,其中使用的辐射测量五个信道的频率为υ1= 10.65 GHz,υ2= 18 7 GHz,υ5= 36.5 GHz水平极化和υ3,4= 23.8 GHz垂直极化和水平极化,对全球卫星和地面测量执行设置过程,从而可以与现有的重构精度相比,在大范围的海洋和大气中所有地理区域的海洋中,其总重构精度Q更高。

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