提出了一种基于拟合优度检验的正交频分复用(Orthogonal Frequency Division Multiplexing,OFDM)系统频谱检测算法.该算法利用OFDM系统循环前缀和被复制数据间相关系数的经验分布与其理论分布之间的距离来进行频谱检测.仿真表明:该检测...提出了一种基于拟合优度检验的正交频分复用(Orthogonal Frequency Division Multiplexing,OFDM)系统频谱检测算法.该算法利用OFDM系统循环前缀和被复制数据间相关系数的经验分布与其理论分布之间的距离来进行频谱检测.仿真表明:该检测算法比基于循环前缀自相关系数检测法具有更好的检测性能,在噪声不确定情况下优于能量检测.展开更多
In this work, Green-Naghdi （GN） equations with general weight functions were derived in a simple way. A wave-absorbing beach was also considered in the general GN equations. A numerical solution for a level higher t...In this work, Green-Naghdi （GN） equations with general weight functions were derived in a simple way. A wave-absorbing beach was also considered in the general GN equations. A numerical solution for a level higher than 4 was not feasible in the past with the original GN equations. The GN equations for shallow water waves were simplified here, which make the application of high level （higher than 4） equations feasible. The linear dispersion relationships of the first seven levels were presented. The accuracy of dispersion relationships increased as the level increased. Level 7 GN equations are capable of simulating waves out to wave number times depth kd 〈 26. Numerical simulation of nonlinear water waves was performed by use of Level 5 and 7 GN equations, which will be presented in the next paper.展开更多
文摘提出了一种基于拟合优度检验的正交频分复用(Orthogonal Frequency Division Multiplexing,OFDM)系统频谱检测算法.该算法利用OFDM系统循环前缀和被复制数据间相关系数的经验分布与其理论分布之间的距离来进行频谱检测.仿真表明:该检测算法比基于循环前缀自相关系数检测法具有更好的检测性能,在噪声不确定情况下优于能量检测.
基金Supported by the Special Fund for Basic Scientific Research of Central Colleges Harbin Engineering University(Harbin)the National Natural Science Foundation of China+1 种基金Doctor Subject Foundation of the Ministry of Education of Chinathe"111"project(B07019)
文摘In this work, Green-Naghdi （GN） equations with general weight functions were derived in a simple way. A wave-absorbing beach was also considered in the general GN equations. A numerical solution for a level higher than 4 was not feasible in the past with the original GN equations. The GN equations for shallow water waves were simplified here, which make the application of high level （higher than 4） equations feasible. The linear dispersion relationships of the first seven levels were presented. The accuracy of dispersion relationships increased as the level increased. Level 7 GN equations are capable of simulating waves out to wave number times depth kd 〈 26. Numerical simulation of nonlinear water waves was performed by use of Level 5 and 7 GN equations, which will be presented in the next paper.
