Add to ORKGVery simple formulae are derived for the difference in mean level between the two sides of a submerged breakwater when waves are incident on it at an arbitrary angle. The formulae apply also to waves undergoing refraction due to changes in depth and to waves in open channel transitions
For the generation of internal waves by long surface waves, the normal-mode equations and solutions ...
The P-V-T properties of seawater calculated from the sound derived equation of state of Wang and Mil...
A simple analysis shows the analogy between Rossby waves and waves caused by irregularities in the d...
Mutual effects of progressive wave motion in shallow water and in underlaying fluid sediments are di...
When a current is crossed by a vessel on fixed course at fixed speed, the vessel is displaced downst...
Mapping of wave trains during four flights over the ocean off southern California showed the consist...
Breakwaters can generally be divided into three categories based on where the sea level is: submerge...
An island of circular cylindrical shape, situated on a paraboloidal shoal (Fig. 1 and Table 1) in an...
This paper considers the response of the sea surface to a low-frequency long-wavelength plane-wave p...
Observations of vertical and horizontal variations in salinity and velocity in the James River estua...
The generation of longshore currents on a beach is investigated theoretically, using the concept of ...
Hayes and Halpern (1976) have calculated the rays associated with internal waves in the semidiurnal ...
The tides on a regular open coast change rapidly as a stonn approaches, and the time history of this...
Waves are reflected whenever they move into a region where their speed of propagation changes. It ha...
Observations made with an array of wave sensors reveal significant differences between the high-freq...
For the generation of internal waves by long surface waves, the normal-mode equations and solutions ...
The P-V-T properties of seawater calculated from the sound derived equation of state of Wang and Mil...
A simple analysis shows the analogy between Rossby waves and waves caused by irregularities in the d...
Mutual effects of progressive wave motion in shallow water and in underlaying fluid sediments are di...
When a current is crossed by a vessel on fixed course at fixed speed, the vessel is displaced downst...
Mapping of wave trains during four flights over the ocean off southern California showed the consist...
Breakwaters can generally be divided into three categories based on where the sea level is: submerge...
An island of circular cylindrical shape, situated on a paraboloidal shoal (Fig. 1 and Table 1) in an...
This paper considers the response of the sea surface to a low-frequency long-wavelength plane-wave p...
Observations of vertical and horizontal variations in salinity and velocity in the James River estua...
The generation of longshore currents on a beach is investigated theoretically, using the concept of ...
Hayes and Halpern (1976) have calculated the rays associated with internal waves in the semidiurnal ...
The tides on a regular open coast change rapidly as a stonn approaches, and the time history of this...
Waves are reflected whenever they move into a region where their speed of propagation changes. It ha...
Observations made with an array of wave sensors reveal significant differences between the high-freq...
For the generation of internal waves by long surface waves, the normal-mode equations and solutions ...
The P-V-T properties of seawater calculated from the sound derived equation of state of Wang and Mil...
A simple analysis shows the analogy between Rossby waves and waves caused by irregularities in the d...