Numerical comparisons of the damping of internal gravity waves in stratified fluids

1970 ◽  
Vol 79 (1) ◽  
pp. 53-65 ◽  
Author(s):  
D. J. Crampin ◽  
B. D. Dore
1978 ◽  
Vol 12 (4) ◽  
pp. 157-165 ◽  
Author(s):  
T. Kubota ◽  
D.R.S. Ko ◽  
L.D. Dobbs

1968 ◽  
Vol 34 (3) ◽  
pp. 609-624 ◽  
Author(s):  
Walter L. Jones

A numerical examination has been made of the reflectivity of critical levels with low Richardson number to internal gravity waves propagating in stratified fluids with shear. At sufficiently low positive Richardson numbers the reflected wave may actually be stronger than the incident.The normal mode instabilities of three simple models have also been computed. The results are presented in three dimensions: Richardson number, horizontal wave scale and real wave frequency.


2001 ◽  
Vol 7 (2s) ◽  
pp. 26-33 ◽  
Author(s):  
O.E. Gotynyan ◽  
◽  
V.N. Ivchenko ◽  
Yu.G. Rapoport ◽  
◽  
...  

2019 ◽  
Vol 4 (1) ◽  
Author(s):  
Alan Brandt ◽  
Kara R. Shipley

2021 ◽  
Vol 921 ◽  
Author(s):  
Christopher J. Howland ◽  
John R. Taylor ◽  
C.P. Caulfield

Abstract


2014 ◽  
Vol 32 (2) ◽  
pp. 181-186 ◽  
Author(s):  
O. Onishchenko ◽  
O. Pokhotelov ◽  
W. Horton ◽  
A. Smolyakov ◽  
T. Kaladze ◽  
...  

Abstract. The effect of the wind shear on the roll structures of nonlinear internal gravity waves (IGWs) in the Earth's atmosphere with the finite vertical temperature gradients is investigated. A closed system of equations is derived for the nonlinear dynamics of the IGWs in the presence of temperature gradients and sheared wind. The solution in the form of rolls has been obtained. The new condition for the existence of such structures was found by taking into account the roll spatial scale, the horizontal speed and wind shear parameters. We have shown that the roll structures can exist in a dynamically unstable atmosphere.


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