Computationally Efficient Formulation of Sparse Color Image Recovery in the JPEG Compressed Domain

2013 ◽  
Vol 49 (1) ◽  
pp. 173-190 ◽  
Author(s):  
Camelia Florea ◽  
Mihaela Gordan ◽  
Aurel Vlaicu ◽  
Radu Orghidan
Author(s):  
Tianheng Zhang ◽  
Jianli Zhao ◽  
Qiuxia Sun ◽  
Bin Zhang ◽  
Jianjian Chen ◽  
...  

2013 ◽  
Vol 8-9 ◽  
pp. 480-489 ◽  
Author(s):  
Camelia Florea ◽  
Mihaela Gordan ◽  
Bogdan Orza ◽  
Aurel Vlaicu

Image filtering is one of the principal tools used in computer vision applications. Real systems store and manipulate high resolution images in compressed forms, therefore the implementation of the entire processing chain directly in the compressed domain became essential. This includes almost always linear filtering operations implemented by convolution. Linear image filtering implementation directly on the JPEG images is challenging for several reasons, including the complexity of transposing the pixel level convolution in the compressed domain, which may increase the processing time, despite avoiding the decompression. In this paper we propose a new computationally efficient solution for JPEG image filtering (as a spatial convolution between the input image and a given kernel) directly in the DCT based compressed domain. We propose that the convolution operation to be applied just on the periodical extensions of the DCT basis images, as an off-line processing, obtaining the filtered DCT basis images, which are used in data decompression. While this doesn't solve the near block boundaries filtering artefacts for large convolution kernels, for most practical cases, it provides good quality results at a very low computational complexity. These kind of implementations can run at real-time rates/ speeds and are suitable for developments of applications on digital cameras/ DSP/FPGA.


Geophysics ◽  
1994 ◽  
Vol 59 (10) ◽  
pp. 1542-1550 ◽  
Author(s):  
Richard S. Smith ◽  
R. N. Edwards ◽  
G. Buselli

Coincident‐loop TEM sounding data are often presented by plotting the half‐space apparent conductivity as a function of delay time. A new algorithm generates an improved presentation that plots the apparent conductivity as a function of depth. The resulting data may be further processed to sharpen or “spike” the smoothly varying apparent‐conductivity/depth curves in an attempt to better represent the rapid changes in conductivity that often exist in the earth. The algorithm described involves an approximation, but is simple, easy to use, and computationally efficient. A layered conductivity structure is assumed, so the algorithm is best for areas where the geology is approximately horizontal. However, the algorithm can also be used to identify anomalous features that are not infinite horizontal layers. The spiked conductivity models derived from synthetic data are consistent with the original layered‐earth models and show a greater resolution than the apparent‐conductivity/depth curves, and sometimes amplify noise in the data. When data are collected along a profile line, the conductivity/depth information can be converted to a color image. For profile data collected over the Elura orebody, the image of the spiked conductivity section shows an anomalous feature at the orebody, and the color contrast is more marked than it is on the apparent‐conductivity/depth image.


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