scholarly journals Random wave propagation theory for intermediate and saturated ranges

1978 ◽  
Vol 64 (S1) ◽  
pp. S22-S23 ◽  
Author(s):  
W. C. Meecham ◽  
H. T. Yura ◽  
M. T. Tavis
Keyword(s):  
Wave Propagation ◽  
Random Wave ◽  
Propagation Theory

Longitudinal Collision of Rod-Rigid Element Systems

1983 ◽  
Vol 50 (3) ◽  
pp. 637-640 ◽  
Author(s):  
A. Mioduchowski ◽  
M. G. Faulkner ◽  
A. Pielorz ◽  
W. Nadolski
Keyword(s):  
Wave Propagation ◽  
Elastic Rods ◽  
Propagation Theory ◽  
One Dimensional ◽  
Rigid Element ◽  
Dimensional Wave

One-dimensional wave propagation theory is used to investigate the forces, velocities, and displacements in a series of elastic rods connected to rigid elements. The method is applied to the case of two subsystems that collide. The technique allows the calculations to be done during a short-lived event such as a collision.

Wave Propagation Theory for Evaluating Dynamic Soil Stress-Strain Models

1988 ◽  
Vol 31 (3) ◽  
pp. 0683-0691 ◽  
Author(s):  
M. F. Kocher ◽  
J. D. Summers
Keyword(s):  
Wave Propagation ◽  
Propagation Theory ◽  
Stress Strain ◽  
Soil Stress

Wave Propagation Theory

2011 ◽  
pp. 65-153 ◽  
Author(s):  
Finn B. Jensen ◽  
William A. Kuperman ◽  
Michael B. Porter ◽  
Henrik Schmidt
Keyword(s):  
Wave Propagation ◽  
Propagation Theory

Teleconnections from Tropics to Northern Extratropics through a Southerly Conveyor

2005 ◽  
Vol 62 (11) ◽  
pp. 4057-4070 ◽  
Author(s):  
Zhuo Wang ◽  
C-P. Chang ◽  
Bin Wang ◽  
Fei-Fei Jin
Keyword(s):  
Wave Propagation ◽  
Rossby Wave ◽  
Rossby Waves ◽  
Propagation Theory ◽  
Wave Source ◽  
Tropical Forcing ◽  
Rossby Wave Source ◽  
Rossby Wave Response ◽  
Rossby Wave Propagation ◽  
The Tropics

Abstract Rossby wave propagation theory predicts that Rossby waves in a tropical easterly flow cannot escape from the Tropics to the extratropics. Here the authors show that a southerly flow component in the basic state (a southerly conveyor) may transfer a Rossby wave source northward; thus, a forcing embedded in the deep tropical easterlies may excite a Rossby wave response in the extratropical westerlies. It is shown that the southerly conveyor determines the location of the effective Rossby wave source and that the extratropical response is relatively insensitive to the location of the tropical forcing, provided that the tropical response can reach the southerly conveyor. A stronger southerly flow favors a stronger extratropical response, and the spatial structure of the extratropical response is determined by the extratropical westerly basic flows.

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