The local similarity algorithm can be used for the calculation of signals of any dimension. For 1D signals, the meanings of equations 13 and 14 are intuitive. For 2D or higher-dimensional signals, each signal is first reshaped into a 1D signal and then follows equations 13 and 14 to calculate the local similarity vector. The smoothing operator is applied to the 2D or multi-dimensional form of the original signal to enforce the smoothness in any dimension. Figures 3 and 4 show demonstrations for both 1D and 2D signals. Figures 3a and 3b show the same trace with different level of noise. Figure 3c shows the calculated local similarity for the 1D signal. Figures 4a and 4b show the same flattened gather with different level of noise. Figure 4c shows the calculated local similarity for the 2D signal. From the two examples, we can conclude that the local similarity can effectively obtain smooth and reasonable measurements for both 1D and 2D signals. The peaks in the calculated local similarity indicate the position of useful wavelets correctly.
trace-comp
Figure 3. Local similarity for 1D signal. (a) & (b) The same trace with different level of noise. (c) Calculated local similarity. |
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flat-comp
Figure 4. Local similarity for 2D signal. (a) & (b) The same flattened gather with different level of noise. (c) Calculated local similarity. |
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