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After applying transformation to the residual signal, the transformed coefficients are further encoded by T/F encoder, and the quantized residual in the previous frame, is obtained as shown in Figure 4(b).
The transformed coefficients of different frequencies are rearranged into three-dimensional (3D) wavelet sub-band structures.
Then, the transformed coefficients are obtained by projecting coefficients through the separate trained models.
In frequency domain, the transformed coefficients of the host image are modified by the watermark image [1].
For these macroblocks with redundant motion vector, there will be no transformed coefficients to be encapsulated in the redundant macroblocks.
Figure 4 shows the real seismic data reconstructed after the threshold filtering of the Wavelet transformed coefficients.
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x n = the transformed coefficient.
fourier descriptors, bidimensional wavelet transform coefficients, bidimensional Fourier transform coefficients, angular-radial transform coefficients.
Fig. 2 Energy distribution of transform coefficients.
(a) Tsukuba transform coefficients following the inter-view transform.
These features are based on: (1) fourier descriptors, (2) bidimensional wavelet transform coefficients, (3) bidimensional Fourier transform coefficients, (4) angular-radial transform coefficients. .
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