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Numerical Simulation and Analysis of the Spiky Sea Clutter from the Sea Surface With Breaking Waves

机译:海面碎波刺浪的数值模拟与分析。

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摘要

This paper presents a feasible and efficient scattering model of the time-varying complex sea surface process to the field of sea spike modeling. To describe the phenomena of sea spikes as well as the “super events” from realistic sea clutter, wedges are posited on the two-scale sea surface to provide an approximate simulation of the breaking waves. The scattering of the wedge and multiple reflections that occur from the sea and wedges are considered in ray tracing for a large HH/VV ratio. With this technique, we obtained the time sequence of the time-varying sea surface and identified the spiking events in the background. Sea clutter properties with breaking waves are compared with that of the sea. Results indicate that spiking events are more likely to occur in the sea with breaking waves. The probability distribution function (PDF) curve of the sea surface with breaking waves has a heavy trail in the large amplitude region. The decorrelation time of the sea with breaking waves is significantly longer compared with the sea without breaking waves, particularly, for HH polarization. The spike properties of sea clutter in different wind speeds and resolutions are also investigated. Results show that spike events are more likely to happen under a high sea state and radar resolution. The Doppler spectrum of the sea with breaking waves showed remarkable improvement for both polarizations. All simulation results indicate that the proposed scattering model effectively stimulates sea clutter with a low grazing incident angle and explains the physical mechanism of the sea spikes.
机译:本文向海峰建模领域提出了一种时变复杂海面过程的可行而有效的散射模型。为了描述海峰现象以及现实海浪杂波中的“超级事件”,在两尺度海面上放置了楔形物,以提供对破碎波的近似模拟。对于大的HH / VV比,在光线跟踪中考虑了楔形物的散射以及海和楔形物产生的多次反射。利用这种技术,我们获得了时变海面的时间序列,并识别了背景中的尖峰事件。将具有破碎波的海杂波特性与海的杂波特性进行比较。结果表明,尖峰事件更有可能在海中爆发。带有破碎波的海面的概率分布函数(PDF)曲线在大振幅区域中具有较重的轨迹。与没有碎波的海相比,具有碎波的海的去相关时间明显更长,特别是对于HH极化而言。还研究了在不同风速和分辨率下海杂波的尖峰特性。结果表明,在高海况和雷达分辨率下,峰值事件更有可能发生。带有碎波的海的多普勒频谱对两种极化均表现出显着改善。所有模拟结果表明,所提出的散射模型有效地激发了低掠入射角的海浪杂波,并解释了海峰的物理机制。

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