Difference between revisions of "INCITE"
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| − | DOE | + | During the past two years, SCEC scientists have used the DOE Oak Ridge and Argonne Leadership Computing Facilities, as well as NSF supercomputers, to develop petascale seismic hazard simulations can provide numerical simulations of the largest earthquakes at frequencies higher than 1 Hz. |
[[File:Anderson |256px|thumb|right|Fig 1:Map of velocity profile lines of interest. Pins represent CyberShake hazard curve sites. GAVI is a precarious rock site and a CyberShake hazard curve site. (Image Credit: John Anderson (UNR))]] | [[File:Anderson |256px|thumb|right|Fig 1:Map of velocity profile lines of interest. Pins represent CyberShake hazard curve sites. GAVI is a precarious rock site and a CyberShake hazard curve site. (Image Credit: John Anderson (UNR))]] | ||
== SCEC INCITE 2010 == | == SCEC INCITE 2010 == | ||
| + | *[http://hypocenter.usc.edu/research/ProgressReports/Jordan_ALCF_CloseOut_2010_Q4_Report.pdf Argonne Leadership Computing Facility 2010 Closeout Report] | ||
| + | *[http://hypocenter.usc.edu/research/ProgressReports/Jordan_OLCF_CloseOut_2010_Q4_Report.pdf Oak Ridge National Lab 2010 Close Out Report] | ||
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| + | == SCEC INCITE 2010 == | ||
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*[http://hypocenter.usc.edu/research/ProgressReports/Jordan_ALCF_CloseOut_2010_Q4_Report.pdf Argonne Leadership Computing Facility 2010 Closeout Report] | *[http://hypocenter.usc.edu/research/ProgressReports/Jordan_ALCF_CloseOut_2010_Q4_Report.pdf Argonne Leadership Computing Facility 2010 Closeout Report] | ||
*[http://hypocenter.usc.edu/research/ProgressReports/Jordan_OLCF_CloseOut_2010_Q4_Report.pdf Oak Ridge National Lab 2010 Close Out Report] | *[http://hypocenter.usc.edu/research/ProgressReports/Jordan_OLCF_CloseOut_2010_Q4_Report.pdf Oak Ridge National Lab 2010 Close Out Report] | ||
Revision as of 01:28, 1 April 2011
During the past two years, SCEC scientists have used the DOE Oak Ridge and Argonne Leadership Computing Facilities, as well as NSF supercomputers, to develop petascale seismic hazard simulations can provide numerical simulations of the largest earthquakes at frequencies higher than 1 Hz.
File:Anderson
Fig 1:Map of velocity profile lines of interest. Pins represent CyberShake hazard curve sites. GAVI is a precarious rock site and a CyberShake hazard curve site. (Image Credit: John Anderson (UNR))
SCEC INCITE 2010
- Argonne Leadership Computing Facility 2010 Closeout Report
- Oak Ridge National Lab 2010 Close Out Report
SCEC INCITE 2010
- Argonne Leadership Computing Facility 2010 Closeout Report
- Oak Ridge National Lab 2010 Close Out Report
Related Entries
- Argonne National Laboratory Leadership Class Computing Facility
- Oak Ridge National Laboratory Leadership Class Computing Facility
- CME Project
- M8
- Full 3D Tomography
- UCVM
- CyberShake
