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mse

于 2008-07-23 发布 文件大小:2KB
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下载积分: 1 下载次数: 148

代码说明:

  采用Matlab编写的最小二乘法,实现对两类的正确分类(Prepared by the use of Matlab least squares method, to realize two types of correct classification)

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  • levelfms
    此应用程序不仅表明了基本的使用Microsoft基础类,而且也是一个起点书面申请。(This application not only demonstrates the basic use of Microsoft Foundation Classes, but also a starting point for an application in writing.)
    2009-05-07 08:02:01下载
    积分:1
  • main2
    说明:  生成正态性检验及界面,可进行完整的正态性检验(Normal test generation and interface, can be a complete test of normality)
    2011-03-18 00:02:22下载
    积分:1
  • rls
    Recursive Least Squares.
    2011-09-22 21:50:17下载
    积分:1
  • LFM10us
    Lfm信号的simulink模块,模拟的是10微秒的信号,已验证(Lfm signal Simulink module, analog signal is 10 microseconds, has been verified)
    2012-02-29 21:40:47下载
    积分:1
  • 一维均匀平行板传输线fdtd序fdtd1
    说明:  一维均匀平行板传输线fdtd程序,使用高斯脉冲激励,mur吸收边界条件(One-dimensional uniform parallel plate transmission line fdtd program, using Gaussian pulse excitation, mur absorption boundary)
    2020-05-12 23:15:46下载
    积分:1
  • zhifangtu
    根据已经给定的数组,按要求绘制直方图的形状(code)
    2009-10-22 10:19:47下载
    积分:1
  • monituihuo
    说明:  用模拟退火的算法解决中国旅行商的问题,结果画出图形直观明了!(Using simulated annealing algorithm to solve traveling salesman problem of China, resulting in intuitive and clear graphics to draw!)
    2009-08-11 16:58:56下载
    积分:1
  • source
    输入信号为方波信号+高斯白噪声,方波信号基 频为1kHz,幅值为1,高斯白噪声方差为0.2, 均值为0,采样频率为20kHz。试用周期图法和 ARMA谱估计法(SVD-TLS)估计此信号的功率 谱,并分析比较其结果(The input signal is a square wave signal+ Gaussian white noise, square wave signal fundamental frequency 1kHz, amplitude is a Gaussian white noise variance is 0.2, the mean is 0, the sampling frequency is 20kHz. Try periodogram and ARMA spectral estimation method (SVD-TLS) estimate the power spectrum of this signal, and the analysis and comparison of the results)
    2013-10-29 17:49:35下载
    积分:1
  • grav_nonlinear
    地球物理勘探中重力资料解释的主要目的是由地表观测值推断地下可能存在的密度分布。众所周知,任何一组重力数据都可能由无数个密度分布所引起。即使假设了重力异常是由具有均匀密度差的单一地质体产生的,也得不出唯一的解(Gravity geophysical exploration data interpretation main purpose is inferred from surface observations may exist underground density distribution. Is known, any set of data may be provided by gravity density caused numerous. Even assuming that the gravity anomaly is determined by having a uniform density difference arising from a single geological body, they have no unique solution)
    2013-11-21 23:46:03下载
    积分:1
  • pf
    标准matlab代码,备有较为详细的注释(Standard Matlab code, with more detailed notes)
    2013-05-10 20:52:53下载
    积分:1
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