雹云微结构的遥感数学模型的建立

Khamisha M. Senov, K. Sabanchiev, Y. Bolgov, I. Nogerov, Raisa I. Elbaeva
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引用次数: 0

摘要

本文讨论了利用冰雹云的雷达反射率测量结果建立数学模型来确定冰雹云微观结构的问题。利用雷达特征确定冰雹云的微结构可归结为求解Fredholm 1类积分方程,该方程属于散射理论的逆问题,属于不适定问题。基于a . N. Tikhonov提出的求解不适定问题的方法,建立了一个数学模型和算法,利用雷达在不同波长的反射率结果求出冰雹粒子的分布函数。三、四、五波长分布函数的计算结果。结果表明,所提出的数学模型和算法具有足够的精度和稳定性,可作为近似求解雷达反射率测量冰雹粒径谱问题的有效工具。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Development of a mathematical model of microstructure of hail clouds by remote sensing
The article is devoted the problem of developing mathematical models for determining the microstructure of hail clouds by results of measurements of radar reflectivity from the hail clouds. Determination of microstructure of hail clouds by radar characteristics is reduced to solving integral equation of Fredholm 1 kind that belongs to the class of inverse problems of scattering theory and is an ill-posed problem. Based on the method of solving ill-posed problems proposed by A. N. Tikhonov, a mathematical model and the algorithm, allowing by results of the radar reflectivity at different wavelengths, to find the distribution function of the hail particles. The results of calculation of distribution functions for three, four and five wavelengths. It is shown that the proposed mathematical model and algorithm has sufficient accuracy and stability and can serve as an effective tool for approximate solution of the problem of finding the spectrum of hail particle size measurement of radar reflectivity.
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