射频干扰(Radio Frequency Interference,RFI)会对高频地波雷达有用回波产生较大影响。本文提出了一种慢时域射频干扰抑制方法,首先利用频谱监测数据实现射频干扰的分段检测,而后基于射频干扰在慢时域的短时相干性、强距离相关性和方向...射频干扰(Radio Frequency Interference,RFI)会对高频地波雷达有用回波产生较大影响。本文提出了一种慢时域射频干扰抑制方法,首先利用频谱监测数据实现射频干扰的分段检测,而后基于射频干扰在慢时域的短时相干性、强距离相关性和方向特性,在常规高阶奇异值分解(Higher-Order Singular Value Decomposition,HOSVD)方法的基础上,结合训练张量三种展开模式矩阵的特点,利用左、右奇异矩阵包含的频率信息实现对干扰子空间的准确估计,进而实现对射频干扰的分段消除。仿真和实测数据的处理结果都表明,该方法可以有效检测并消除射频干扰,提高了数据批处理的运算效率。展开更多
为实现对高频地波雷达(high frequency surface wave radar,HFSWR)一阶海杂波谱中目标的检测,提出了基于奇异值分解(singular value decomposition,SVD)的空域海杂波抑制算法(简称空域SVD算法).空域SVD算法是利用海杂波较强的相关性,将...为实现对高频地波雷达(high frequency surface wave radar,HFSWR)一阶海杂波谱中目标的检测,提出了基于奇异值分解(singular value decomposition,SVD)的空域海杂波抑制算法(简称空域SVD算法).空域SVD算法是利用海杂波较强的相关性,将邻近距离单元作为参考,对其阵列协方差矩阵进行SVD,估计空域的海杂波子空间和噪声子空间;再利用子空间的正交性,从阵列回波信号中去除其在海杂波子空间的投影分量,达到在空域抑制海杂波的目的.该方法与现有的空域海杂波抑制方法相比,不需要预先知道海杂波的方位,利用阵列协方差矩阵的SVD来估计子空间,使得子空间的估计比较容易且准确,提高了输出信杂噪比(signal to clutter plus noise ratio,SCNR),有利于目标的检测.展开更多
高频地波雷达的探测性能极易受到射频干扰的影响,当前射频干扰抑制的研究主要是通过人工识别来逐一处理,鲜见实时自动识别与抑制射频干扰的研究。随着深度学习在雷达图像处理方面应用的展开,本文尝试将其引入高频雷达射频干扰抑制中,利...高频地波雷达的探测性能极易受到射频干扰的影响,当前射频干扰抑制的研究主要是通过人工识别来逐一处理,鲜见实时自动识别与抑制射频干扰的研究。随着深度学习在雷达图像处理方面应用的展开,本文尝试将其引入高频雷达射频干扰抑制中,利用YOLO(You Only Look Once)模型来识别雷达距离多普勒谱图中的射频干扰,继而用高阶奇异值分解(Higher Order Singular Value Decomposition,HOSVD)方法对其进行抑制。仿真和实测数据处理结果表明,此YOLO-HOSVD联合算法实现了对高频雷达射频干扰的自动识别与抑制,单场数据处理时间不超过1.8 s。该方法可以应用于高频地波雷达常规海态观测。展开更多
A detection method of offshore area depth utilizing the x-band microwave radar is proposed. The method is based on the sea clutter imaging mechanism of microwave radar, and combined with dispersion equation of the lin...A detection method of offshore area depth utilizing the x-band microwave radar is proposed. The method is based on the sea clutter imaging mechanism of microwave radar, and combined with dispersion equation of the liner wave theorem and least square method (LSM), consequently get the inversion results of water depth in the detected region. The wave monitoring system OSMAR-X exploited by the Ocean State Laborato-ry, Wuhan University, based on a microwave radar has proven to be a powerful tool to monitor ocean waves in time and space. Numerical simulation and inversion of offshore area depth are carried out here; since JONSWAP model can give description of stormy waves in different growth phase, it is suitable for simulation. Besides, some results from measured data detected by OSMAR-X x-band radar located at Longhai of Fujian Province, China, validates this method. The tendency of the average water depths inferred from the radar images is in good agreement with the tide level detected by Xiamen tide station. These promising results suggest the possibility of using OSMAR-X to monitor operationally morphodynamics in coastal zones. This method can be applied to both shore-based and shipborne x-band microwave radar.展开更多
Based on the quasi-harmonic analysis of 11 d vector ocean currents obtained from two high frequency sur- face wave radars located at Zhujiajian Island and Shengshan Island, the spatial distribution characteristics of ...Based on the quasi-harmonic analysis of 11 d vector ocean currents obtained from two high frequency sur- face wave radars located at Zhujiajian Island and Shengshan Island, the spatial distribution characteristics of surface tidal currents in the open sea area to the east of the Zhoushan Islands of Zhejiang Province, China are studied. The following conclusions are drawn from the analysis: the tidal current pattern in the open sea area to the east of Zhoushan Islands is primarily regular semidiurnal, which is significantly affected by the shallow water constituents. The directions of the major axes of tidal current ellipses of M2 lie approx- imately in the NW-SE direction. With the increasing of distance away from the coast, the directions of the tidal current ellipses gradually shift toward the E-W direction. The tidal currents are mainly reversing cur- rents. The spatial distribution of probable maximum current velocities decreases gradually from northeast to southwest which is basically in accordance with the spatial distribution of measured maximum current velocities. The residual currents near the coast are larger than those far away from the coast. The directions of the residual currents are basically north by east, and the angle to the due north increases gradually with the increasing distance away from the coast. The topography shows a certain impact on the spatial distri- bution of shallow water constituents, the rotation of tidal currents, the probable maximum currents and the residual currents.展开更多
为抑制海杂波检测高频地波雷达(high frequency surface wave radar,HFSWR)中的目标,提出了基于零陷展宽(null widening,NW)的空域海杂波抑制算法.NW算法利用海洋运动的连续性和海杂波的弥散性,基于干扰位置变化规律构造加权干扰NW矩阵...为抑制海杂波检测高频地波雷达(high frequency surface wave radar,HFSWR)中的目标,提出了基于零陷展宽(null widening,NW)的空域海杂波抑制算法.NW算法利用海洋运动的连续性和海杂波的弥散性,基于干扰位置变化规律构造加权干扰NW矩阵,从阵列中抑制海杂波并保留目标.与其他海杂波抑制算法对比,利用新的波束形成方法将干扰零陷方向展宽,不改变噪声项贡献,从而有效抑制海杂波.利用NW算法在空域抑制海杂波时,根据实际应用环境计算修正矩阵,在实时信号处理过程中不仅运算速度快,而且提高了输出信号杂波噪声比(signal to clutter plus noise ratio,SCNR),针对海杂波抑制效果较好,有助于后续信号处理目标检测工作.展开更多
文摘射频干扰(Radio Frequency Interference,RFI)会对高频地波雷达有用回波产生较大影响。本文提出了一种慢时域射频干扰抑制方法,首先利用频谱监测数据实现射频干扰的分段检测,而后基于射频干扰在慢时域的短时相干性、强距离相关性和方向特性,在常规高阶奇异值分解(Higher-Order Singular Value Decomposition,HOSVD)方法的基础上,结合训练张量三种展开模式矩阵的特点,利用左、右奇异矩阵包含的频率信息实现对干扰子空间的准确估计,进而实现对射频干扰的分段消除。仿真和实测数据的处理结果都表明,该方法可以有效检测并消除射频干扰,提高了数据批处理的运算效率。
文摘为实现对高频地波雷达(high frequency surface wave radar,HFSWR)一阶海杂波谱中目标的检测,提出了基于奇异值分解(singular value decomposition,SVD)的空域海杂波抑制算法(简称空域SVD算法).空域SVD算法是利用海杂波较强的相关性,将邻近距离单元作为参考,对其阵列协方差矩阵进行SVD,估计空域的海杂波子空间和噪声子空间;再利用子空间的正交性,从阵列回波信号中去除其在海杂波子空间的投影分量,达到在空域抑制海杂波的目的.该方法与现有的空域海杂波抑制方法相比,不需要预先知道海杂波的方位,利用阵列协方差矩阵的SVD来估计子空间,使得子空间的估计比较容易且准确,提高了输出信杂噪比(signal to clutter plus noise ratio,SCNR),有利于目标的检测.
文摘高频地波雷达的探测性能极易受到射频干扰的影响,当前射频干扰抑制的研究主要是通过人工识别来逐一处理,鲜见实时自动识别与抑制射频干扰的研究。随着深度学习在雷达图像处理方面应用的展开,本文尝试将其引入高频雷达射频干扰抑制中,利用YOLO(You Only Look Once)模型来识别雷达距离多普勒谱图中的射频干扰,继而用高阶奇异值分解(Higher Order Singular Value Decomposition,HOSVD)方法对其进行抑制。仿真和实测数据处理结果表明,此YOLO-HOSVD联合算法实现了对高频雷达射频干扰的自动识别与抑制,单场数据处理时间不超过1.8 s。该方法可以应用于高频地波雷达常规海态观测。
基金The National High Technology Research and Development Program(863 Program)of China under contract No.2012AA091701the Specialized Research Fund for the Doctoral Program of Higher Education of China under contract No.2014212020203
文摘A detection method of offshore area depth utilizing the x-band microwave radar is proposed. The method is based on the sea clutter imaging mechanism of microwave radar, and combined with dispersion equation of the liner wave theorem and least square method (LSM), consequently get the inversion results of water depth in the detected region. The wave monitoring system OSMAR-X exploited by the Ocean State Laborato-ry, Wuhan University, based on a microwave radar has proven to be a powerful tool to monitor ocean waves in time and space. Numerical simulation and inversion of offshore area depth are carried out here; since JONSWAP model can give description of stormy waves in different growth phase, it is suitable for simulation. Besides, some results from measured data detected by OSMAR-X x-band radar located at Longhai of Fujian Province, China, validates this method. The tendency of the average water depths inferred from the radar images is in good agreement with the tide level detected by Xiamen tide station. These promising results suggest the possibility of using OSMAR-X to monitor operationally morphodynamics in coastal zones. This method can be applied to both shore-based and shipborne x-band microwave radar.
基金The National High Technology Research and Development Program of China(863 Program)under contract No.2012AA091701the Fundamental Research Fund for the Central Universities of China under contract No.2012212020211
文摘Based on the quasi-harmonic analysis of 11 d vector ocean currents obtained from two high frequency sur- face wave radars located at Zhujiajian Island and Shengshan Island, the spatial distribution characteristics of surface tidal currents in the open sea area to the east of the Zhoushan Islands of Zhejiang Province, China are studied. The following conclusions are drawn from the analysis: the tidal current pattern in the open sea area to the east of Zhoushan Islands is primarily regular semidiurnal, which is significantly affected by the shallow water constituents. The directions of the major axes of tidal current ellipses of M2 lie approx- imately in the NW-SE direction. With the increasing of distance away from the coast, the directions of the tidal current ellipses gradually shift toward the E-W direction. The tidal currents are mainly reversing cur- rents. The spatial distribution of probable maximum current velocities decreases gradually from northeast to southwest which is basically in accordance with the spatial distribution of measured maximum current velocities. The residual currents near the coast are larger than those far away from the coast. The directions of the residual currents are basically north by east, and the angle to the due north increases gradually with the increasing distance away from the coast. The topography shows a certain impact on the spatial distri- bution of shallow water constituents, the rotation of tidal currents, the probable maximum currents and the residual currents.
文摘为抑制海杂波检测高频地波雷达(high frequency surface wave radar,HFSWR)中的目标,提出了基于零陷展宽(null widening,NW)的空域海杂波抑制算法.NW算法利用海洋运动的连续性和海杂波的弥散性,基于干扰位置变化规律构造加权干扰NW矩阵,从阵列中抑制海杂波并保留目标.与其他海杂波抑制算法对比,利用新的波束形成方法将干扰零陷方向展宽,不改变噪声项贡献,从而有效抑制海杂波.利用NW算法在空域抑制海杂波时,根据实际应用环境计算修正矩阵,在实时信号处理过程中不仅运算速度快,而且提高了输出信号杂波噪声比(signal to clutter plus noise ratio,SCNR),针对海杂波抑制效果较好,有助于后续信号处理目标检测工作.