Can Rossby Waves in the Ocean Create Vortices?

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Rossby waves in the atmosphere are known to create low-pressure areas and spawn vortices, leading to cyclones. The discussion raises the possibility of similar phenomena occurring in the ocean, questioning whether oceanic Rossby waves can also generate vortices and their potential size. It is noted that atmospheric cyclones arise from smaller-scale turbulence within Rossby waves, while oceanic circulations may exhibit less turbulence due to lower Reynolds numbers, attributed to the higher viscosity of water compared to air. The conversation highlights the observation of large systems, sometimes up to 1000 miles in diameter, which can become stationary and are often associated with Rossby waves. The relationship between these waves, the super systems they may influence, and other atmospheric conditions remains a point of inquiry, particularly regarding the sequence of events that lead to these phenomena.
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Rossby waves in the atmosphere spawn vortices which are low pressure areas.

Is it possible that the Rossby waves in the ocean spawn vortices? If so, how big might they be?

Something tells me that I'm not going to get an answer to this question.
 
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Understanding very little of that topic I nevertheless dare to express some thoughts on it:
In atmosphere the creation of cyclones is due to smaller scale turbulences being embedded in the Rossby waves. I suppose that the oceanic circulations are much less turbulent on comparable length scales as the Reynolds numbers are much lower due to the higher viscosity of water as compared to air.
 
Yes, see

Oceanography by Summerhayes and Thorpe, p67
 
I'm watching for systems 1000 miles in diameter. Often they become stationary and all hell breaks loose. When they become stationary, there is often a Rossby Wave associated with the system. Which comes first: the Rossby Wave, the Super System, the temp/inverted Troposphere, an abnormal stationary updraft?
 
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