Accuracy of the explicit planar free-surface boundary condition implemented in a fourth-order staggered-grid velocity-stress finite-difference scheme

Citation
E. Gottschammer et Kb. Olsen, Accuracy of the explicit planar free-surface boundary condition implemented in a fourth-order staggered-grid velocity-stress finite-difference scheme, B SEIS S AM, 91(3), 2001, pp. 617-623
Citations number
15
Categorie Soggetti
Earth Sciences
Journal title
BULLETIN OF THE SEISMOLOGICAL SOCIETY OF AMERICA
ISSN journal
00371106 → ACNP
Volume
91
Issue
3
Year of publication
2001
Pages
617 - 623
Database
ISI
SICI code
0037-1106(200106)91:3<617:AOTEPF>2.0.ZU;2-Y
Abstract
We compute the accuracy of two implementations of the explicit planar free- surface boundary condition for 3D fourth-order velocity-stress staggered-gr id finite differences, 1/2 grid apart vertically, in a uniform half-space. Due to the staggered grid, the closest distance between the free surface an d some wave-field components for both implementations is 1/2-grid spacing, Overall, the differences in accuracy of the two implementations are small. When compared to a reflectivity solution computed at the staggered position s closest to the surface, the total misfit for all three components of the wave field is generally found to be larger for the free surface colocated w ith the normal stresses, compared to that for the free surface colocated wi th the xz and yz stresses. However, this trend is reversed when compared to the reflectivity solution exactly at the free surface (the misfit encounte red in staggered-grid modeling). When the wave field is averaged across the free surface, thereby centering the staggered wave field exactly on the fr ee surface, the free-surface condition colocated with the xz and yz stresse s generates the smallest total misfit for increasing epicentral distance. F or an epicentral distance/hypocentral depth of 10, the total misfit of this condition is about 15% smaller than that for the condition colocated with the normal stresses, mainly controlled by the misfit on the Rayleigh wave.