The fully staggered grid (FSG) combines multiple standard staggered grids (SSGs) to simulate seismic wave propagation in anisotropic elastic media. However, its accuracy is contingent upon the wavefield’s consistency and continuity across multiple sets of SSGs. In isotropic or weakly anisotropic media, decoupling or weak coupling between the SSGs can lead to wavefield discontinuities at adjacent grid points in the diagonal direction. Issues such as inconsistent source activation, medium parameter discontinuities, and different numerical treatments of boundary conditions over multiple sets of SSGs can exacerbate these problems. While previous methods, such as FD-consistent point source technique and equivalent medium parameterization methods, have partially addressed these issues, they do not completely solve the problem. This study, drawing inspiration from numerical damping techniques used in collocated-grid finite-difference schemes to eliminate odd-even oscillations, introduces an explicit filter operator along the diagonal direction of the FSG. This approach ensures wavefield consistency and continuity across multiple SSGs, improving the accuracy of the FSG scheme. Although this method increases computational costs, it is essential for reliable seismic modeling in anisotropic media.
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