Abstract
Low-frequency (LF) cargo ship wake is a major source of hydrodynamic energy in shipping channels, where it has increasingly been linked to shoreline erosion. The LF wake consists of a drawdown called the “Bernoulli depression,” a return surge, and finally a series of trailing waves that may persist longer than 30 minutes after the vessel passage. While the Bernoulli depression and surge are well-explained by conservation principles, we presently lack a robust explanation of the trailing waves. They are a ubiquitous feature observed at many locations (e.g. Garrel, Lopez, and Collins, 2008), and have frequently been attributed to cross-channel seiching; however, field measurements from the Savannah River, GA, USA suggested that some of the waves may have alongshore progressive characteristics, which contradicts this assumption.References
Garel, Lopez, and Collins (2008): Sediment resuspension events induced by the wake wash of deep-draft vessels, Geo-Marine Letters, vol. 28, issue 4, pp. 215-211.
Haas and Muscalus (2019): Bird-Long Island Management Study Phase 1B: Hydrodynamic Characterizations for Bird/Long Island. No, FHWA-GA-19-1634. Georgia Department of Transportation.
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