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Gui
matlab编程代码中的GUI设计非常有用,都是初级设计，希望有说帮助，(some design about matlab gui)
- 2011-12-20 09:26:00下载
- 积分：1
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xsk_rd1
sar雷达成像算法仿真，希望有高手指点一下！(sar radar imaging algorithm simulation, you would like to have expert advice!)
- 2007-05-24 14:52:04下载
- 积分：1
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samson2018720pblurayx264ytsag-english-128177
ojdojdojdj ndijdijidj bdjbdjbdjb jbjbdjbdjb
- 2019-01-24 02:16:45下载
- 积分：1
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Frequency_sel_channel_est_equa
This codes are for frequency selective fading channels for MIMO system. Both estimation and equalization are done using LS and MMSE estimation and ZF and MMSE equalization.
- 2015-02-11 19:34:01下载
- 积分：1
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diansanshe
点散射方法进行混响仿真，信号为单频信号，散射体高斯分布，无多普勒频域(Reverberation simulation, signal point scattering method for single-frequency signal, the scattering body Gaussian distribution)
- 2012-11-01 21:00:59下载
- 积分：1
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自适应观测器故障诊断
利用自适应观测器进行故障诊断，matlab仿真，修改参数即可(Using adaptive observer for fault diagnosis, matlab simulation, modify the parameters can be)
- 2021-03-03 11:29:33下载
- 积分：1
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firdesign
This document is astep by step guide to design digital filters using matlab
- 2009-04-27 21:26:22下载
- 积分：1
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duane1
This program performs the Duane growth method with least-squares fit of an input data set to a straight line
- 2011-02-02 02:33:23下载
- 积分：1
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winOnTop
windows on plot tool box
- 2012-04-24 16:37:45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
