Discussion Overview
The discussion centers on the potential relationship between Rossby waves in the ocean and the formation of vortices. Participants explore the mechanisms involved, the scale of these vortices, and the differences between atmospheric and oceanic dynamics.
Discussion Character
- Exploratory, Technical explanation, Debate/contested
Main Points Raised
- One participant questions whether Rossby waves in the ocean can create vortices and speculates on their potential size.
- Another participant suggests that while cyclones in the atmosphere are formed by smaller scale turbulences within Rossby waves, oceanic circulations may be less turbulent due to lower Reynolds numbers resulting from water's higher viscosity.
- A reference to a specific oceanography text is provided, indicating that there may be established discussions on the topic.
- A participant describes observing large systems (1000 miles in diameter) that become stationary and suggests a possible connection to Rossby waves, raising questions about the sequence of events leading to these systems.
Areas of Agreement / Disagreement
The discussion contains multiple competing views and remains unresolved regarding the relationship between Rossby waves and oceanic vortices.
Contextual Notes
Participants express varying levels of understanding and assumptions about the turbulence in oceanic versus atmospheric systems, which may affect their claims. The discussion does not clarify the definitions or conditions under which Rossby waves and vortices are being considered.