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The Transmission and Decay of Barotropic Topographic Rossby Waves Incident on a Continental Shelf
Barotropic Topographic Rossby Waves Continental Shelf
2009/3/7
We know that long-period (>1 day) and long-wavelength (>100 km) topographical Rossby waves can be generated by a wind acting directly on a continental shelf (Adams and Buchwald, 1969). Here we examine...
On the Propagation of Free Topographic Rossby Waves near Continental Margins. Part 2：Numerical Model
Numerical Model Continental Margins Free Topographic Rossby Waves
2009/2/18
Ou (1980, Part 1) presented analytical solutions of free topographic Rossby waves propagating in an infinite wedge filled with a uniformly stratified fluid. We present here in Part 2 a numerical model...
On the Propagation of Free Topographic Rossby Waves near Continental Margins. Part 1：Analytical Model for a Wedge
Free Topographic Rossby Waves Continental Margins Wedge
2009/2/18
An analytical model has been constructed to study the propagation of free waves of subinertial frequency in an infinite wedge filled with a uniformly stratified fluid. The problem is found to transfor...
The Effect of Current Shear on Topographic Rossby Waves
Current Shear Topographic Rossby Waves
2009/2/16
Topographic Rossby waves are long-period waves which occur on continental slopes. In this paper we examine the effect of a mean current on these waves, when the current is directed along the isobaths ...
The Kinetic Energy on a Continental Shelf from Topographic Rossby Waves Generated off the Shelf
Kinetic Energy Topographic Rossby Waves Continental Shelf
2009/2/13
Over a deep barotropic ocean an isolated pressure cell, producing a wind stress curl, generates topographic Rossby waves which are incident on a continental shelf with a simple exponentially varying s...
Topographic Rossby Waves off East Australia：Identification and Role in Shelf Circulation
Topographic Rossby Waves East Australia Shelf Circulation
2009/2/11
Hamon et al.(1975) analyzed two years of surface current data from ships' set along two tracks parallel to 560 km of the east Australian shelf and found a phase lag of 10 days between long (120 day) p...
Observations of Topographic Rossby Waves on the Continental Margin off Nova Scotia
Topographic Rossby Waves Continental Margin Nova Scotia
2009/2/7
Bursts of topographic-Rossby-wave energy have been observed in data recorded by an array of current meters moored on the outer continental shelf and slope off Nova Scotia north of the Gulf Stream. The...
A Numerical Study of the Propagation of Topographic Rossby Waves
Topographic Rossby Waves shelf waves
2009/1/7
The propagation of linear barotropic Rossby waves is investiaged numerically over a one-dimensional topography similar to the continental rise and slope. A point source is used to generate waves with ...
Gulf Stream–Generated Topographic Rossby Waves
topographic Rossby waves Gulf Stream continental slope
2008/12/11
An inverse ray tracing model is applied to observations of 40-day topographic Rossby waves on the continental slope off of Cape Hatteras, North Carolina, to determine their origin. The rays are traced...
Deep Eddy Energy and Topographic Rossby Waves in the Gulf of Mexico
Deep Eddy Energy Topographic Rossby Waves Gulf of Mexico
2008/6/25
Observations suggest the hypothesis that deep eddy kinetic energy (EKE) in the Gulf of Mexico can be accounted for by topographic Rossby waves (TRWs). It is presumed that the TRWs are forced by Loop C...