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Simulating Supercell Storms and Tornaodes in Unprecedented Detail and Accuracy

Simulating Supercell Storms and Tornaodes in Unprecedented Detail and Accuracy. Bob Wilhelmson bw@ncsa.uiuc.edu Professor, Atmospheric Sciences Chief Scientist, NCSA Atmospheric Science Storm Group (DAS) Advanced Visualization Laboratory (NCSA).

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Simulating Supercell Storms and Tornaodes in Unprecedented Detail and Accuracy

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  1. Simulating Supercell Storms and Tornaodes in Unprecedented Detail and Accuracy Bob Wilhelmson bw@ncsa.uiuc.edu Professor, Atmospheric Sciences Chief Scientist, NCSA Atmospheric Science Storm Group (DAS) Advanced Visualization Laboratory (NCSA)

  2. Animation from simulation data ( ~ 1 terabyte) Nominated for an Academy Award, 1989

  3. NCSA’s Stereo 4K and Stereo HD Theater with Video Playback

  4. NOVA Supercell and Tornado Evolution Imaginations unbound

  5. PRAC: Understanding Tornadoes and Their Parent Supercells Through Ultra-High Resolution Simulation/Analysis Bob Wilhelmson (UIUC), et al • Goal • Simulate development, structure, & demise of large damaging tornadoes in supercells at resolution sufficient to capture low-level tornado inflow, thin precipitation shaft that forms “hook echo” adjacent to tornado, and other smaller scale structures • Approach • Simulate storms with model that solves (using finite differences) the equations of motion for air and water substances (droplets, rain, ice, …)

  6. Tornadoes (cont’d) • Approach continued: • Explore new numerical algorithms that will more effectively use multicore architecture of Blue Waters • Address load balancing issues that arise from the fact that the microphysics only operates in regions where clouds are forming or are present • In-situ data analysis will be carried out whenever possible due to large data volumes • Grids ranging from 5,000 x 5,000 x 1,000 to 10,000 x 10,000 x 2,000 grid points, the latter with 10 m uniform resolution within the storm • Sustained petascale simulation will require > 3 days on full system Simulated tornado-like path with a 50 mb pressure drop extending from the ground to a height of 6 km using 100 m horizontal resolution

  7. Tornadoes (cont’d) • Application Code • CM1 (Cloud Model, from George Bryan, NCAR) Fortran, MPI/OpenMP • Bottlenecks to Scalability • Load imbalance in the microphysics as some cells have cloud and others do not • Sound wave propagation algorithm takes small steps, few FLOPS per memory fetch • Percentage of Peak • 6.25% on Power 6; 92% parallel efficiency from 32 to 512 cores • Development Plan for Application Improvements • Improve performance of dynamics code and scale advection scheme or change some of the algorithms for better scaling • Add dynamic load balancing of microphysics • Overlap computation with communication • Perform on-the-fly data analysis/visualization including use of trajectories to deal with the 10’s of petabytes of data from a single simulation

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