2008
DOI: 10.1007/978-3-540-87475-1_41
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Benchmark Study of a 3d Parallel Code for the Propagation of Large Subduction Earthquakes

Abstract: Abstract. Benchmark studies were carried out on a recently optimized parallel 3D seismic wave propagation code that uses finite differences on a staggered grid with 2 nd order operators in time and 4 th order in space. Three dual-core supercomputer platforms were used to run the parallel program using MPI. Efficiencies of 0.91 and 0.48 with 1024 cores were obtained on HECToR (UK) and KanBalam (Mexico), and 0.66 with 8192 cores on HECToR. The 3D velocity field pattern from a simulation of the 1985 Mexico earthq… Show more

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Cited by 3 publications
(6 citation statements)
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“…An important result of those studies was that, even though theoretically the computed synthetic seismograms (Cabrera, et al, 2007;Chavez et al, 2008) for the 0.5 and 0.25-km spatial discretization should have a frequency content larger than 1 Hz, the Fourier amplitude spectra of the corresponding synthetics had very small values at a frequency of ∼0:3 Hz (< 0:5 Hz) for all the previously mentioned space and temporal discretizations. This result is in agreement with Mendoza and Hartzell (1989), who emphasized the 0.5-Hz limit of their source inversion.…”
Section: Modeling Resultsmentioning
confidence: 99%
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“…An important result of those studies was that, even though theoretically the computed synthetic seismograms (Cabrera, et al, 2007;Chavez et al, 2008) for the 0.5 and 0.25-km spatial discretization should have a frequency content larger than 1 Hz, the Fourier amplitude spectra of the corresponding synthetics had very small values at a frequency of ∼0:3 Hz (< 0:5 Hz) for all the previously mentioned space and temporal discretizations. This result is in agreement with Mendoza and Hartzell (1989), who emphasized the 0.5-Hz limit of their source inversion.…”
Section: Modeling Resultsmentioning
confidence: 99%
“…The 3DOPFD code previously has been successfully used to obtain near-field and far-field low-frequency synthetics of the 19 September 1985 M s 8.1 Michoacan, Mexico, earthquake (Cabrera, et al, 2007;Chavez et al, 2008). For those studies, the authors used the slip distribution suggested by Mendoza and Hartzell (1989), who, for the source inversion of the 1985 Michoacan event, used nearfield and teleseismic waveform data low-pass filtered at 0.5 Hz and utilized 120 subfaults of 15 × 13:9 km 2 , each of them to obtain the slip distribution of the event.…”
Section: Modeling Resultsmentioning
confidence: 99%
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