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An Improved Empirical Model for Radar Sea Clutter Reflectivity

机译:雷达海杂波反射率的改进经验模型

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摘要

A fundamental characteristic of radar sea clutter, important for radar performance evaluations, is its apparent reflectivity defined as $sigma??$ ($m^2/m^2$). "Apparent" is used as a reminder that any measurement of sea clutter reflectivity includes the effects of propagation and shadowing close to the sea surface. Sea clutter reflectivity depends on many factors, including sea state, wind velocity, grazing angle, polarization, and radar frequency. An empirical sea clutter model proposed by Horst, et al. (1978), the so-called GIT model, has found widespread acceptance in the radar community. However, this model does not always agree with what is the most complete experimental database of sea clutter reflectivity available to the radar systems engineer. The 1991 edition of F. E. Nathanson's book provides seven tables of measured sea clutter reflectivity data summarized from approximately 60 sources. The large deviation between the GIT model and this database, in particular at lower sea states, has prompted NRL to develop an improved model for sea clutter reflectivity based on these tables. The model is a function of radar frequency, polarization, sea state, and grazing angle. The functional form of this empirical model was chosen such that the average absolute deviation (in dB) between the model and the experimental data was minimized.
机译:雷达海杂波的基本特征对雷达性能评估很重要,其视在反射率定义为$ sigma ?? $($ m ^ 2 / m ^ 2 $)。 “表观”用于提醒您,任何对海杂波反射率的测量都包括靠近海面的传播和阴影效应。海杂波反射率取决于许多因素,包括海况,风速,掠射角,极化和雷达频率。 Horst等人提出的经验性海杂波模型。 (1978年),即所谓的GIT模型,已在雷达界得到广泛接受。但是,该模型并不总是与雷达系统工程师可获得的最完整的海杂波反射率实验数据库一致。内森森(F. E. Nathanson)的1991年版提供了七个表,这些表总结了大约60种来源的海杂波反射率数据。 GIT模型与该数据库之间的较大偏差,尤其是在低海状态下,促使NRL根据这些表开发了一种改进的海杂波反射率模型。该模型是雷达频率,极化,海况和掠射角的函数。选择该经验模型的功能形式,以使模型与实验数据之间的平均绝对偏差(以dB为单位)最小。

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