无线电引信海面后向散射系数仿真分析

针对无线电引信在海杂波背景下目标检测问题的需要,在分析入射余角、工作频率、极化方式以及海面状态对后向散射系数影响的基础上,给出了海杂波对引信信杂比的影响,并对Morchin模型和双尺度粗糙面复合模型两类海面后向散射模型进行仿真和拟合;仿真结果表明:在大入射余角条件下,较双尺度粗糙面复合模型,Morchin模型能够取得更好的拟合效果,更有效地反映无线电引信超低空工作时海面后向散射系数。

空天双基地雷达海杂波建模与分析

空天双基地雷达作为一种新兴的天基雷达体制,发射机置于卫星上,接收机采用飞行器,极大地克服了传统单基地天基雷达空间传输损耗过大的问题,但其杂波特性更加复杂。对空天双基地雷达海杂波特性进行了分析,首先分析了空天双基地雷达的几何构型,然后基于海杂波双基散射系数和运动特性因素构建了海杂波空时数学模型,最后结合理论与仿真结果阐释了空天双基海杂波特性,为空天双基地雷达杂波抑制技术研究提供了参考。

Sea Surface Roughness Derivation from Wind Speed Estimated by Satellite Altimeter

For open sea conditions the sea surface roughness is described as a function of surface stress and wind speed over sea surface by Charnock relation. The sea surface roughnessn in the North-west Pacific Ocean is derived successfully using wind speed data estimated by the TOPEX satellite altimeter. From the results we find that： （1） the mean sea surface roughness in winter is greater than in summer; （2） compared with other sea areas, the sea surface roughness in the sea area east of Japan （ N30°- 40°, E135°- 150°） is larger than in other sea areas; （3） sea surface roughness in the South China Sea changes more greatly than that in the Bohai Sea, Yellow Sea and East China Sea.