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Phase jump due to partial reflection of irregular water waves at steep slopes
The process of wave breaking at steep slopes is inextricably linked with the simultaneous formation of a reflected wave and a transmit-ted wave pulse corresponding to run-up. According to the law of conservation of momentum the water level deflection of the reflected wave must be negative, while the transmitted run-up is positive. Superimposition of incident and reflected waves results in the formation of a partial clapotis comprising of an imperfect node at the slope face, which is an indicator of a phase jump.
Phase jump due to partial reflection of irregular water waves at steep slopes
The process of wave breaking at steep slopes is inextricably linked with the simultaneous formation of a reflected wave and a transmit-ted wave pulse corresponding to run-up. According to the law of conservation of momentum the water level deflection of the reflected wave must be negative, while the transmitted run-up is positive. Superimposition of incident and reflected waves results in the formation of a partial clapotis comprising of an imperfect node at the slope face, which is an indicator of a phase jump.
Phase jump due to partial reflection of irregular water waves at steep slopes
Büsching, Fritz (Autor:in)
COASTLAB 10
International Conference on the Application of Physical Modelling to Port and Coastal Protection
[Short version]
2010
Online Ressource (PDF-Dokument: 10 S.)
Konferenzband
Elektronische Ressource
Englisch
Phase jump due to partial reflection of irregular water waves at steep slopes
| UB Braunschweig | 2010
The runup and reflection of solitary waves on steep slopes
| TIBKAT | 1991