The Physics of Storm Surge Inundation
Coastal surge results from the interaction of atmospheric barometric pressure drops, sustained onshore winds, and shallow bathymetric shelving.
1. Coupled Hydrodynamic and Wave Physics
The Advanced Circulation (ADCIRC) model coupled with Simulating Waves Nearshore (SWAN) accurately models wave setup—the increase in mean water level due to the breaking of wind-driven waves along shorelines.
2. Boundary Condition Inputs
Atmospheric forcing requires precise Holland wind field formulations and NOAA water level station calibration. Even minor shifts in landfall angle create dramatic non-linear variations in peak surge height.
3. Designing Hardened Defense Infrastructure
Model outputs guide crest elevation specifications for seawalls, revetments, and living shoreline wetlands to protect critical coastal assets.