Far fields of internal gravity waves in a stratified liquid of varying depth

2013 ◽  
Vol 49 (3) ◽  
pp. 329-333 ◽  
Author(s):  
V. V. Bulatov ◽  
Yu. V. Vladimirov
1972 ◽  
Vol 56 (4) ◽  
pp. 721-740 ◽  
Author(s):  
D. G. Hurley

The paper describes a simple but general method for solving 'steady-state’ problems involving internal gravity waves in a stably stratified liquid. Under the assumption that the motion is two-dimensional and that the Brunt-Väisälä frequency is constant, the method is used to re-derive in a very simple way the solutions to problems where the boundary of the liquid is either a wedge or a circular cylinder. The method is then used to investigate the effect that a model of the continental shelf has on an incident train of internal gravity waves. The method involves analytic continuation in the frequency of the disturbance, and may well prove to be effective for other types of wave problem.


1967 ◽  
Vol 28 (1) ◽  
pp. 1-16 ◽  
Author(s):  
D. E. Mowbray ◽  
B. S. H. Rarity

Experiments were conducted to test the linear theory of internal gravity waves produced in a stably stratified liquid by the forced oscillations and the initial impulsive motion of a two-dimensional stationary disturbance. The measurements of the wave configuration in a medium whose density increased linearly with depth were made by means of a Toepler-schlieren system. The agreement between observation and prediction was found to be good.


Oceanology ◽  
2018 ◽  
Vol 58 (6) ◽  
pp. 796-801 ◽  
Author(s):  
V. V. Bulatov ◽  
Yu. V. Vladimirov

1967 ◽  
Vol 30 (3) ◽  
pp. 489-495 ◽  
Author(s):  
D. E. Mowbray ◽  
B. S. H. Rarity

Experiments were conducted to test the linear theory of internal gravity waves produced in a stably stratified liquid by the steady vertical motion of a sphere. The measurements of the phase configuration in a medium whose density increased linearly with depth were made by means of a Toepler-schlieren system. The agreement between observation and prediction was found to be good.


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