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dbf_mvdr
最小方差无畸变响应波束形成器，MVDR算法源码(The minimum variance distortionless response beamformer，MVDR algorithm source
)
- 2012-06-05 22:43:54下载
- 积分：1
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cordic-matlab
cordic向量迭代求取IQ信号幅值，及相位
反cordic求正弦、余弦值(use cordic to computer the magnitude of IQ signal and cos、sin )
- 2014-10-21 14:06:50下载
- 积分：1
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XIJIAOdfig
西交硕士毕业论文_双馈风力发电机DFIG,包括模型的搭建方法,仿真结果分析等等.(Xi' an Jiaotong Master' s Thesis _ doubly-fed wind generator DFIG model structures, analysis of simulation results.)
- 2013-04-27 20:26:23下载
- 积分：1
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Pss-stability
power system stability with and without PSS yu power system stability book example
- 2014-01-27 18:55:58下载
- 积分：1
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25707
数值积分 romberg matlab编程(Numerical integration romberg matlab programming)
- 2009-11-28 17:19:56下载
- 积分：1
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polyphase
这个是多相滤波的MATLAB程序，做接收机的同学可以参考的(this is a polyphase programme)
- 2013-11-06 20:01:53下载
- 积分：1
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EqVsIFFT
DVB-T 2K signal generation Eq. (2.1.4) vs. 2N-IFFT.DVB-T 2K 信号发生器matlab源代码。(DVB-T 2K signal generation Eq. (2.1.4) vs. 2N-IFFT.DVB-T 2K signal generator matlab source code.)
- 2008-05-15 13:58:03下载
- 积分：1
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RLSwangsave
针对现场工业数据，实现状态空间模型的递推最小二乘算法的辨识(For on-site industrial data to achieve state-space model identification recursive least squares algorithm)
- 2013-08-21 11:42:05下载
- 积分：1
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cordic_EasyMatlab
自己编的Matlab实现旋转模式的CORDIC代码，附对应的参考资料，一看就懂。(Matlab realize their series rotation mode CORDIC code, with corresponding reference data, one can understand.)
- 2013-08-29 18:56:01下载
- 积分：1
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matlab-raytrace
射线追踪,包含了起点和终点的射线函数，对于地震传播研究具有重要意义！(Raytracing in a v(z) world. The toolbox contains functions forshooting fans of rays and functions for tracing rays with specific start and end points. General multi-bounce rays with any number of mode conversions can be traced. Automatic routines for P-P and P-S primaries in shot-gather geometry are provided for convenience. Any recording geometry can be used but most functions
vectorize (e.g. are most efficient) for shot-gather geometry. Only
traveltimes and rayparameters are detemined, not amplitudes. In these routines, the velocity models should be considered as "background" models. This means that the depths at which flections and mode conversions occur are dependent of the depths given as layer boundaries in the velocity models. Velocity models are specified by a vector of velocities and a same-size vector of depths. The j th velocity is in effect from the j th to the j+1 th depth.
The bottom of the model is assumed at infinite depth. Thus v=5000
and z=0 specifies a cons)
- 2013-09-16 08:15:48下载
- 积分：1
