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1
说明： Amir Hossein Omidvarnia用matlab编写的基于PCA的人脸识别系统和基于FLD的人脸识别系统,其中
的图像示例为Essex face database中 face94 的部分图像,文献可参考"Eigenfaces vs. Fisherfaces:
Recognition using class specific linear projection."已经测试过程序可正常运行没有问题。(Amir Hossein Omidvarnia prepared using matlab Face Recognition System Based on PCA and FLD-based face recognition systems, which sample the image of Essex face database for ' face94' part of images, documents may refer to " Eigenfaces vs. Fisherfaces: Recognition using class specific linear projection. " procedures have been tested there is no problem to normal operation.)
- 2009-07-30 20:41:29下载
- 积分：1
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test_algorithm_menu
说明： TURBO译码性能AWGN信道测试（菜单式）
达到误帧限即可停止当前SNR点的测试，节省计算量(TURBO AWGN channel decoding performance test (menu type) to stop the current error frame is limited to the test SNR point, saving computation)
- 2011-03-09 16:01:14下载
- 积分：1
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CG
说明： 数值分析中没经预处理的高斯方法、经SSOR预处理的高斯方法、经多项式预处理的高斯方法matlab程序(Numerical analysis did not pretreated Gauss method, the SSOR pre-Gaussian method, the pre-Gaussian polynomial method matlab program)
- 2011-08-24 21:50:44下载
- 积分：1
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DSPview4
a fifth version of Dsp view code in matlab
- 2013-10-31 18:34:11下载
- 积分：1
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REG_I_EMF
Matlab simulation of the back efm effect.
- 2009-11-05 17:30:27下载
- 积分：1
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ADCReport
ADC report Matlab implementation
- 2011-01-25 06:30:01下载
- 积分：1
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bbb
用matlab实现三次NURBS插值曲线拟合，插值源程序(Using matlab to achieve Cubic NURBS interpolation curve fitting, interpolation source)
- 2011-08-17 15:50:34下载
- 积分：1
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zuidas
讲述了最大熵估计的方法，以及dsp的实现方法，比较清楚(spoke of the estimated maximum entropy method, and the realization dsp, more clearly)
- 2007-04-23 21:18:17下载
- 积分：1
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gmm3.m
高斯混合模型的核心计算方法，matlab里可直接调用(Core calculation method based on Gaussian mixture model, matlab years can be called directly)
- 2014-10-04 12:55:08下载
- 积分：1
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Wave-in-Viscoelastic-Media
硕士论文：粘弹性介质地震波数值模拟。
震波在实际地层介质中传播与在理想的完全弹性介质中传播有许多不同之处，地层的粘滞性会损耗地震波能量，使其振幅衰减并且视频率逐渐降低。地震波的这种能量
衰减和频散，使得不能直接从地震数据上得到准确的地下信息和分辨率更高的图像。实
际的地层更接近于粘弹性介质，本论文主要探讨和研究了粘弹性介质中地震波传播的数
值模拟方法及其衰减规律。
(Thesis: viscoelastic medium seismic wave numerical simulation. The shock wave propagation in the formation medium and ideal perfectly elastic medium spread there are many differences, the viscosity of the strata will loss seismic energy, so that the amplitude attenuation and video rate gradually reduce. This energy of the seismic wave attenuation and dispersion makes accurate subsurface information and higher resolution images can not be obtained directly from the seismic data. Actual formation closer viscoelastic medium, this thesis is to explore and study the numerical simulation of seismic wave propagation in viscoelastic media and its decay law.)
- 2013-03-01 23:10:56下载
- 积分：1
