Annual Meeting - SCEC.org
Annual Meeting - SCEC.org
Annual Meeting - SCEC.org
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Poster Abstracts | Group 1 – CME/PetaSHA<br />
initialization. Further code enhancements are highly required to meet the novel challenges that<br />
emerge when running at the largest scales.<br />
We ported and optimized the AWP-Olsen code for use on the 504 teraflops TACC’s Ranger<br />
machine. Special algorithms have been implemented into the code for easy adaptation on different<br />
TeraGrid platforms, which proven to be highly effective for use. The optimizations are adjusted at<br />
run-time depending on system characteristics. Additional options are also added to selectively<br />
decimate the output spatially or/and temporally.<br />
Scaling the reads of initial conditions is a challenging task due to its extraordinary size and highly<br />
discontinuous distribution. We have implemented MPI-IO for both source and media initialization.<br />
The parallelization and integration of these routines involves first determining the layout of the<br />
physical cells that describes physical velocity information and the sources that provide fault<br />
information to processors in a manner that can be used by the IO routines. Based on the precalculated<br />
information, linear abstract data types for both files are created. Each processor can<br />
access its local data linearly with the aforementioned customized MPI-IO data types. Temporal<br />
source partitioning for the source data has also been introduced to prevent a memory buffer<br />
overflow, which may occur when a large amount of source nodes are allocated in a single<br />
processor. The initial parallel mesh initialization has already shown a time reduction from previous<br />
15 hours to less than minute. Further tests are under way for different compilers and large data<br />
sets.<br />
Furthermore, we implemented an application-initiated check-pointing facility to prepare multipleday<br />
ShakeOut-D mesh initialization on three SDSC BG/L racks. This IBM-based restart library<br />
feature is at system-level, where no application-level restart capability is available. This provided<br />
an initial insight of the type of fault tolerance feature needed for petascale computing.<br />
1-021<br />
SEARCHING FOR 3D WAVE-PROPAGATION EFFECTS IN SOUTHERN<br />
CALIFORNIA Ely GP<br />
Ground motions in southern California can be significantly influenced by three-dimensional basin<br />
wave-propagation effects. Amplification due to focusing was observed in Santa Monica during the<br />
1994 Northridge event. Simulations of large events on the southern San Andreas within the <strong>SCEC</strong><br />
Community Velocity Model (CVM) find large amplifications at Whittier Narrows due to basinguided<br />
waves. We have begun a study to search for similar basin effects in southern California,<br />
using a series 3D wave-propagation simulations over a suite of potential source scenarios. Selection<br />
of scenarios is being guided by the Uniform California Earthquake Rupture Forecast, as well as<br />
CyberShake--an effort to estimate probabilistic seismic hazard based on 3D simulations.<br />
Simulations will be performed up to 0.5 Hz using the Support Operator Rupture Dynamics (SORD)<br />
code and kinematic finite-fault sources, with fault geometry (often non-planar) from the <strong>SCEC</strong><br />
Community Fault Model. Waves will be propagated through the <strong>SCEC</strong>-CVM as well as the <strong>SCEC</strong>-<br />
CVMH (Harvard version) with comparisons helping to address uncertainty in the basin effect<br />
results. Selected scenarios will recomputed with dynamic rupture sources.<br />
1-022<br />
WEBSIMS: A PYTHON-BASED WEB APPLICATION FOR STORING, EXPLORING<br />
AND DISSEMINATING 4D EARTHQUAKE SIMULATION DATA Ely GP, and Olsen KB<br />
WebSims aims to provide a tool for cataloging, exploring, comparing and sharing four-dimensional<br />
results of large numerical earthquake simulations. Users may extract time histories or two-<br />
78 | Southern California Earthquake Center