Planetary Upstream Waves

Author(s):  
C. T. Russell
Keyword(s):  
1990 ◽  
Vol 17 (13) ◽  
pp. 2293-2296 ◽  
Author(s):  
D. S. Orlowski ◽  
G. K. Crawford ◽  
C. R. Russell
Keyword(s):  

1969 ◽  
Vol 39 (3) ◽  
pp. 433-442 ◽  
Author(s):  
John W. Miles

The question of whether or not waves exist upstream of an obstacle that moves uniformly through an unbounded, incompressible, inviscid, unseparated, rotating flow is addressed by considering the development of the disturbed flow induced by a weak, moving dipole that is introduced into an axisymmetric, rotating flow that is initially undisturbed. Starting from the linearized equations of motion, it is shown that the flow tends asymptotically to the steady flow determined on the hypothesis of no upstream waves and that the transient at a fixed point is O(1/t). It also is shown that the axial velocity upstream (x < 0) of the dipole as x → − ∞ with t fixed is O(|x|−3), as in potential flow, but is O(|x|−1) as t → ∞ with |x| fixed. The results extend directly to closed obstacles of sufficiently small transverse dimensions and suggest the existence of a finite, parametric domain of no upstream waves for smooth, slender obstacles. The axial velocity in front of a small, moving sphere at a given instant in the transient régime is calculated and compared with Pritchard's laboratory measurements. The agreement is within the experimental scatter for Rossby numbers greater than about 0·3 even though the equivalence between sphere and dipole is exact only for infinite Rossby number.


1994 ◽  
Vol 263 ◽  
pp. 293-318 ◽  
Author(s):  
Hideshi Hanazaki

A numerical study of the three-dimensional internal waves excited by topography in the flow of a stratified fluid is described. In the resonant flow of a nearly two-layer fluid, it is found that the time-development of the nonlinearly excited waves agrees qualitatively with the solution of the forced KP equation or the forced extended KP equation. In this case, the upstream-advancing solitary waves become asymptotically straight crested because of abnormal reflection at the sidewall similar to Mach reflection. The same phenomenon also occurs in the subcritical flow of a nearly two-layer fluid. However, in the subcritical flow of a linearly stratified Boussinesq fluid, the two-dimensionalization of the upstream waves can be interpreted as the separation of the lateral modes due to the differences in the group velocity of the linear wave, although this does not mean in general that the generation of upstream waves is describable by the linearized equation.


1986 ◽  
Vol 6 (1) ◽  
pp. 85-88
Author(s):  
C.T. Russell ◽  
J.G. Luhmann ◽  
R.C. Elphic ◽  
D.J. Southwood

1994 ◽  
Vol 99 (A1) ◽  
pp. 169 ◽  
Author(s):  
D. S. Orlowski ◽  
C. T. Russell ◽  
D. Krauss-Varban ◽  
N. Omidi

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