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ON RADAR IMAGING OF OCEAN PHENOMENA

机译:关于海洋现象的雷达成像

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A model of radar imaging of ocean phenomena isrnproposed. This model is an extension of the backgroundrnNRCS model [7] in the case of non-uniform medium.rnRadar scattering component takes into account Braggrnand non-Bragg (specular reflections and the impact ofrnwave breaking) scattering mechanisms. Varying surfacerncurrent, surface temperature (stability effects), andrnsurfactants are the main sources of medium nonuniformities.rnTransformation of wave spectrum andrnwave breaking in non-uniform medium is described inrnthe relaxation approximation. Model calculations arerncompared with field observations. An overall goodrnagreement is obtained. It is shown that wave breakingrnplay important role in the formation of radar signaturesrnof ocean phenomena.
机译:提出了海洋现象的雷达成像模型。在非均匀介质的情况下,该模型是背景rnCS模型的扩展[7]。rnRadar散射分量考虑了Braggrn和非Bragg(镜面反射和rnwave破碎的影响)散射机制。表面电流,表面温度(稳定性效应)和表面活性剂的变化是介质不均匀性的主要来源。弛豫近似描述了在非均匀介质中波谱的转变和波的破裂。模型计算与现场观察相比较。获得了总体共识。结果表明,破波在形成雷达特征海洋现象中起着重要作用。

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