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SCEC/CME Project - How Earthquake Simulations Drive Middleware Requirements : SCEC/CME Project - How Earthquake Simulations Drive Middleware Requirements Philip Maechling SCEC IT Architect 24 June 2005


Southern California Earthquake Center : Southern California Earthquake Center Consortium of 15 core institutions and 39 other participating organizations, founded as an NSF STC in 1991 Co-funded by NSF and USGS under the National Earthquake Hazards Reduction Program (NEHRP) Mission: Gather data on earthquakes in Southern California Integrate information into a comprehensive, physics-based understanding of earthquake phenomena Communicate understanding to end-users and the general public to increase earthquake awareness and reduce earthquake risk Core Institutions University of Southern California (lead) California Institute of Technology Columbia University Harvard University Massachusetts Institute of Technology San Diego State University Stanford University U.S. Geological Survey (3 offices) University of California, Los Angeles University of California, San Diego University of California, Santa Barbara University of Nevada, Reno Participating Institutions 39 national and international universities and research organizations http://www.scec.org


Recent Earthquakes In California : Recent Earthquakes In California


Observed Areas of Strong Ground Motion : Observed Areas of Strong Ground Motion


Simulations Supplement Observed Data : Simulations Supplement Observed Data


SCEC/CME Project : SCEC/CME Project Goal: To develop a cyberinfrastructure that can support system-level earthquake science – the SCEC Community Modeling Environment (CME) Support: 5-yr project funded by the NSF/ITR program under the CISE and Geoscience Directorates Start date: Oct 1, 2001 SCEC/ITR Project NSF CISE GEO SCEC Institutions IRIS USGS ISI SDSC Information Science Earth Science www.scec.org/cme


SCEC/CME Scientific Workflow Construction : SCEC/CME Scientific Workflow Construction A major SCEC/CME objective is the ability to construct and run complex scientific workflow for SHA 9000 Hazard Curve files (9000 x 0.5 Mb = 4.5Gb) Extract IMR Value Plot Hazard Map Lat/Long/Amp (xyz file) with 3000 datapoints (100Kb) Calculate Hazard Curves Gridded Region Definition IMR Definition ERF Definition Probability of Exceedence and IMR Definition GMT Map Configuration Parameters Define Scenario Earthquake Pathway 1 example


SCEC/CME Scientific Workflow System : SCEC/CME Scientific Workflow System


SCEC/CME SRB-based Digital Library : SCEC/CME SRB-based Digital Library SRB-based Digital Library More than 100 Terabytes of tape archive 4 Terabytes of on-line disk 5 Terabytes of disk cache for derivations


Slide10 : Component Library Workflow Template Editor (CAT) Workflow Template (WT) Query for data given metadata L. Hearn @ UBC K. Olsen @ SDSU Execution requirements I/O data descriptions COMPONENTS J. Zechar @ USC (Teamwork: Geo + CS) Domain Ontology Workflow Library Metadata Catalog Conceptual Data Query Engine (DataFinder) Data Selection D. Okaya @ USC Query for WT Workflow Instance (WI) Workflow Mapping (Pegasus) Executable Workflow Grid information services Grid Query for components INTEGRATED WORKFLOW ARCHITECTURE Engineer Tools Tools


SCEC/CME HPC Allocations : SCEC/CME HPC Allocations SCEC/CME researchers have need and have access to significant High Performance Computing capabilities TeraGrid Allocations (April 2005 – March 2006) TG-MCA03S012 (Olsen) 1,020,000 SUs TG-BCS050002S (Okaya) 145,000 Sus USC HPCC Allocations CME Group Allocations (Maechling) 100,000 SUs Investigator Allocations (Li, Jordan) 300,000 SUs SCEC Cluster Dedicated Pentium 4 16 Processor Cluster (102 GFlops)


SCEC/CME TeraGrid Support : SCEC/CME TeraGrid Support TeraGrid Strategic Application Collaboration (SAC) greatly improved our AWM run-time on TeraGrid Advanced TeraGrid Support (ATS) for TeraShake 2 and CyberShake simulations SDSC Visualization Services support for SCEC simulations.


Three Types of Simulations : Three Types of Simulations SCEC/CME supports widely varying types of earthquake simulations Each Simulation type creates it’s own set of middleware requirements Will Describe three examples and comment on their middleware implications and on computational system requirements: Probabilistic Seismic Hazard Maps 3D Waveform Propagation Simulations 3D Waveform-based Intensity Measure Relationship


Slide14 : Probabilistic Seismic Hazard Maps


Example Hazard Curve : Example Hazard Curve Site: USC ERF: Frankel-02 IMR: Field IMT: Peak Velocity Time Period: 50 Years


Probabilistic Hazard Map Calculations : Probabilistic Hazard Map Calculations


Characteristic of PSHA Simulations : Characteristic of PSHA Simulations 10k Independent hazard curve calculations for each map calculations. High throughput, not high performance, computing problem. 10k resulting files per map Metadata saved for each file Short run times on each calculation Overhead of starting up job is expensive. Would like to offer map calculations as service to SCEC users (who may not have an allocation)


Middleware Implications : Middleware Implications High throughput scheduling Well Suited to Condor Pool Bundling of short run-time jobs will reduce job startup overhead. Bundling of jobs useful for clusters execution. Metadata tracking with a RDBMS-based catalog system (e.g. Metadata Catalog System (MCS) and Replication Location Service (RLS) Databases present installation and operational problems at ever site we request them Software support for interpreted language on Computational Clusters Implemented in an interpreted programming language On-demand execution by non-allocated user


3D Wave Propagation Simulations : 3D Wave Propagation Simulations


Characteristics of 3D Wave Propagation Simulations : Characteristics of 3D Wave Propagation Simulations More physically realistic than existing PSHA but more computationally expensive. High Performance Computing, cluster-based codes 4D data calculations (time varying volumetric data) Output large volumetric data sets Physics limited by resolution of grid. Higher ground motion frequencies require denser grid. Double of density increases storage by factor of 8.


Example: TeraShake Simulation : Example: TeraShake Simulation Magnitude 7.7 earthquake on southern San Andreas Mesh of ~2 billion cubes, dx=200 m 0.011 sec time step, 20,000 time steps: 3 minute simulation Kinematic source (from Denali) from Cajon Creek to Bombay Beach 60 sec source duration 18,886 point sources, each 6,800 time steps in duration 240 processors at San Diego SuperComputer Center DataStar ~ 20,000 CPU hours, approximately 5 days wall clock ~ 50 Tbytes of output During execution 'on-the-fly' graphics (…attempt aborted!) Metadata capture and storage in the SCEC digital library


Domain Decomposition For TeraShake Simulations : Domain Decomposition For TeraShake Simulations


Simulations Supplement Observed Data : Simulations Supplement Observed Data


Peak Velocity : Peak Velocity NW-SE Rupture SE-NW rupture


Slide25 : Montebello: 337 cm/s Downtown: 52 cm/s Long Beach: 48 cm/s San Diego: 8 cm/s Palm Springs: 36 cm/s Montebello: 8 cm/s Downtown: 4 cm/s Long Beach: 9 cm/s San Diego: 6 cm/s Palm Springs: 23 cm/s SE-NW NW-SE


Break-down of output : Break-down of output


Middleware Implications for 3D Wave Propagation Simulations : Middleware Implications for 3D Wave Propagation Simulations Multi-day high performance runs Check point restart support needed Schedule reservations on clusters Reservations and special queues are often arranged. Large file and data movement TeraByte transfers require high reliably, long term, data transfers Ability to stop and restart Can we move restart from one system to another Draining of temporary storage during runs Storage required for full often exceeds capability of scratch, so output files must be moved during simulation


Middleware Implications for 3D Wave Propagation Simulations : Middleware Implications for 3D Wave Propagation Simulations On the fly visualization for rapid validation of results Verify before full simulation is completed Standard protocols for data transfers, and metadata registration into SRB-based storage


Slide29 : Waveform-based Intensity Measure Relationship (CyberShake)


Slide30 : Intensity-Measure Relationship List of Supported IMTs List of Site-Related Ind. Params IMT, IML(s) Site(s) Rupture Attenuation Relationships Simulation IMRs exceed. prob. computed using a suite of synthetic seismograms Vector IMRs compute joint prob. of exceeding multiple IMTs (Bazzurro andamp; Cornell, 2002) Multi-Site IMRs compute joint prob. of exceeding IML(s) at multiple sites (e.g., Wesson andamp; Perkins, 2002) Various IMR types (subclasses) Gaussian dist. is assumed; mean and std. from various parameters


CyberShake Simulations Push Macro and Micro Computing : CyberShake Simulations Push Macro and Micro Computing CyberShake requires large forward wave propagation simulations, volumetric data storage CyberShake requires 100k seismogram synthesis computations using multi-Terabyte volumetric data sets. During synthesis processing, this data needs to be disk-based. 100k of data files, and metadata, files to be managed High throughput requirements are driving implementation toward TeraGrid wide computing approach. High throughput requirements are driving integration of non-TeraGrid grids with TeraGrid


Example CyberShake Region (200km x 200km) : Example CyberShake Region (200km x 200km) USC: 34.05,-118.24 minLat=31.889, minLon=-120.60, maxLat=36.1858, maxLon=-115.70


CyberShake Strain Green Tensor AWM : CyberShake Strain Green Tensor AWM Large (TeraShake Scale) forward calculations for each site. SHA typically ignore rupture andgt; 200km from site, so this is used as cutoff distance. 20km buffer distance is used around edges of volume to reduce edge effects 65km depth to support frequencies of interest Volume is 440km x 440km x 65km at 200m spacing 1.573 Billion mesh pts Simulation time 240 seconds Volumetric Data Saved for 2 horizontal simulations Estimated Storage per site is: 7 TB (4.5 data 2.5 checkpoint files)


Ruptures in ERF within 200KM of USC : Ruptures in ERF within 200KM of USC 43227 Ruptures in Frankel02 ERF with M 5.0 or larger within 200km of USC


CyberShake Computational Elements : CyberShake Computational Elements


CyberShake Seismogram Synthesis : CyberShake Seismogram Synthesis Requires calculation of 100,000+ seismogram for each site. Estimate Rupture Variations scale by magnitude: Mw 5.0 x 1 = 20,450 Mw 6.0 x 10 = 216,990 Mw 7.0 x 100 = 106,900 Mw 8.0 x 1000 = 9,000 ------------------ 353,340 Ruptures x 2 components Current estimated number of seismogram files per site is 43,000 (due to combining components and variations into single file per rupture).


CyberShake Seismogram Synthesis : CyberShake Seismogram Synthesis Seismogram synthesis stage requires disk-based data storage of large volumetric data sets so tape based archive of volumetric data sets does not work. To distribute seismogram synthesis across TeraGrid, we need to either duplicate TB of data, or have global visibility on disks systems


Example Hazard Curve : Example Hazard Curve Site: USC ERF: Frankel-02 IMR: Field IMT: Peak Velocity Time Period: 50 Years


Workflows run Using Grid VDS Workflow Tools : Workflows run Using Grid VDS Workflow Tools


Examples Hazard Map Region (50km x 50km at 2km grid spacing = 625 sites) : Examples Hazard Map Region (50km x 50km at 2km grid spacing = 625 sites) OpenSHA SA 1.0 Frankel 2002 ERF and Sadigh with 10% POE in 50 years.


Summary of SCEC Experiences : Summary of SCEC Experiences As soon as we develop a computational capability, the geophysicists develop application that push the technology. Compute technology, data management technology, resource sharing technology all are applied. In many ways, IT capabilities required for geophysical problems exceed what is currently possible and limit the state of knowledge in geophysics and public safety. For example, higher frequency simulations, are of significant interest, but exceed computational and storage capabilities currently available.


Major Middleware related issues for SCEC/CMESecurity and Allocation Management : Major Middleware related issues for SCEC/CME Security and Allocation Management No widely accepted CA makes adding organizations to SCEC grid problematic. Ability to run under group allocations for 'on demand' requests. (Community Allocation ?)


Major Middleware related issues for SCEC/CMESoftware Installation and Maintenance : Major Middleware related issues for SCEC/CME Software Installation and Maintenance Middleware software stack, even at supercomputer systems, support should include micro jobs support such as Java. Database management support for database-oriented tools such as Metadata Catalogs are important (backup, recovery, cleanup, performance, modifications) Guidelines for tools in middleware software stack, should describe when local installations are required and when remote installations are acceptable for tools such as RLS and MCS


Major Middleware related issues for SCEC/CMESupercomputing and Storage : Major Middleware related issues for SCEC/CME Supercomputing and Storage Globally (TeraGrid – wide) visible disk storage Well supported, reliable file transfers with monitoring and restart of jobs with problems are essential. Interoperability between grid tools and data management tools such as SRB must include data and metadata and metadata search.


Major Middleware related issues for SCEC/CMEScheduling Issues : Major Middleware related issues for SCEC/CME Scheduling Issues Support for Reservation-based scheduling Partial run and restart capability Failure detection and alerting


Major Middleware related issues for SCEC/CMEUsability Related and Monitoring : Major Middleware related issues for SCEC/CME Usability Related and Monitoring Monitoring tools that include status of available storage resources. On-the-fly visualizations for run-time validation of results Interfaces to workflow systems are complex, developer oriented interfaces. Easier to user interfaces needed