Large Wave at Daytona Beach, Florida, Explained as a Squall-line Surge

Asburry H Sallenger, Jr., Jeffrey H List, Guy Gelfenbaum, Richard P Stumpf

Abstract


On a clear calm evening during July 1992, an anomalously large wave, reportedly 6 m high, struck the Daytona Beach, Florida area. We hypothesize that a squall line and associated pressure jump, traveling at the speed of a free gravity wave, coupled resonantly with the sea surface forming the large wave or "squall-line surge." The wave was forced along the length of the squall line, with the greatest amplitude occurring at the water depth satisfying the resonant condition. Radar observations showed a strong squall line moving at a steady speed for several hundred kilometers parallel, to the coast from Georgia towards central Florida. The squall line dissipated 10 km north of Daytona Beach; any forced wave would then propagate freely and refract. Wave refraction analyses predict a longshore distribution of wave heights consistent with field measurements of maximum wave runup.

Keywords


Freak waves; overwash; forced wave; wave runup.

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