Gordon Bell Prize Awarded for Cascadia Tsunami Forecasting Breakthrough 

Announcement

The project team receiving the award at the annual Supercomputing Conference (SC25) on November 20, 2025.

About the Gordon Bell Prize

Previous winners have included teams that used exascale supercomputers to design next-generation laser-driven particle accelerators and to perform mesh-refined plasma simulations for advanced accelerators, as well as groups that developed quantum-scale simulations of heat flow in nanoscale transistors and HPC frameworks to study pandemic-scale virus evolution.

In other words, this is a big deal! This prize typically goes to work that defines what’s possible on the most powerful supercomputers in the world and it is very exciting to see Earth Science applications being recognized in this context. 

This Year’s Winning Work: A Digital Twin for Tsunami Early Warning

Digital twin means a computational replica of a real geophysical system that combines physics-based models with observations in real time to estimate its evolving state and explore plausible futures. 

The team combines a fully coupled 3D acoustic-gravity wave model of the ocean with a Bayesian inference framework that ingests seafloor pressure data and, in fractions of a second, estimates seafloor motion and forecasts tsunami heights and timing, including uncertainties, for specific coastal sites. 

The model domain and its unstructured finite element mesh as well as snapshots of the deformation and wave propagation for a moment magnitude 8.7 rupture (modified from Henneking et al., 2025).

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Why This Matters for CRESCENT

Learn More and Celebrate the Team

Videos

Source: Vertical seafloor uplift and seafloor normal velocity from a physics-based 3D dynamic rupture and seismic wave propagation computation (Glehman et al., 2025) of a magnitude 8.7 earthquake scenario spanning the full margin of the Cascadia subduction zone.
Forward Model: Sea bottom pressure and surface wave height computed with a coupled acoustic–gravity 3D wave propagation model, implemented in MFEM, for a magnitude 8.7 earthquake scenario spanning the full margin of the Cascadia subduction zone.
Inverse Solution: Solution of a PDE-based Bayesian inverse problem showing the seafloor normal displacement (truth vs inferred) for a magnitude 8.7 earthquake scenario spanning the full margin of the Cascadia subduction zone. The seafloor motion is inferred in real time from synthetic, noisy data at 600 hypothesized sea bottom pressure sensors.
Art of HPC: An artistic rendering of data from the seafloor normal velocity (source) and the acoustic-gravity model outputs, which was featured as part of SC25’s Art of HPC exhibit.

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