-
Image_Fusion_Toolkit
这是国外研究小波图像处理的学者做出的工具箱,十分好用。(This is the overseas research scholars of wavelet image processing toolbox to make very easy to use.)
- 2009-11-03 09:41:08下载
- 积分:1
-
powerflow-genetical.gorithm
用matlab编写的遗传算法结合潮流计算的程序(Matlab prepared using genetic algorithm combined with the trend of the calculation procedure)
- 2009-05-20 09:20:41下载
- 积分:1
-
利用matlab求解其散射截面消光截面和吸收截面Mie-Matlab-Maetzler-v2
金属小球的米氏散射,利用matlab求解其散射截面消光截面和吸收截面(Mie scattering metal ball, using matlab to solve the scattering and absorption extinction cross-section )
- 2020-07-06 10:58:58下载
- 积分:1
-
dbfread
dbf数据的读取,可用于高频数据处理,比如股票的分时、分笔、逐笔数据(read dbf data, can be used for high frequency data processing)
- 2011-11-23 21:55:35下载
- 积分:1
-
Projet_LMS
My project program LMS, very good
- 2009-03-29 12:54:25下载
- 积分:1
-
cx6_1
振动信号频域处理方法___ 随机信号谱分析(Vibration Frequency Domain Analysis of ___ random signal spectrum)
- 2011-05-06 16:16:01下载
- 积分:1
-
range_compress
线性调频信号的脉冲压缩 线性调频信号的脉冲压缩(chirps sign)
- 2020-11-15 13:59:42下载
- 积分:1
-
fdtd-1D-2D-3D
1,2,3维有限时域差分用于计算电磁学matlab代码!(1,2,3 Dimension Finite Difference Time Domian for EM)
- 2012-12-18 20:36:06下载
- 积分:1
-
matlab1
说明: MATLAB关于一维插值和二维插值学习实例(MATLAB on the one-dimensional interpolation and two-dimensional interpolation example learning)
- 2009-08-22 12:07:38下载
- 积分:1
-
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