Document Type
Article
Publication Date
3-6-2015
Abstract
We demonstrate that ships of moderate size, sailing at low depth Froude numbers (0.37–0.5) in a navigation channel surrounded by shallow banks, produce depressions with depths up to 2.5 m. These depressions (Bernoulli wakes) propagate as long-living strongly nonlinear solitary Riemann waves of depression substantial distances into Venice Lagoon. They gradually become strongly asymmetric with the rear of the depression becoming extremely steep, similar to a bore. As they are dynamically similar, air pressure fluctuations moving over variable-depth coastal areas could generate meteorological tsunamis with a leading depression wave followed by a devastating bore-like feature.
DOI
10.1016/j.physleta.2014.12.004
Recommended Citation
Parnall, K.E. et al. "Ship-Induced Solitary Riemann Waves of Depression in Venice Lagoon." Physics Letters A 379.6 (2015): 555-559.
Included in
Oceanography and Atmospheric Sciences and Meteorology Commons, Terrestrial and Aquatic Ecology Commons
Comments
Version posted is the In Press, Corrected Proof, Available online 8 December 2014.