How Would Ocean Currents Flow on a Smooth Sphere?

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SUMMARY

The discussion centers on the hypothetical scenario of ocean currents on a perfectly smooth, ocean-covered sphere. Participants highlight that ocean currents are primarily driven by salinity differences and temperature variations, particularly in the northern hemisphere. Surface currents flow from the equator towards higher latitudes, influenced by the Coriolis effect, while deeper currents move from the poles towards the equator. Understanding these dynamics is essential for grasping the complexities of real-world ocean currents.

PREREQUISITES
  • Understanding of oceanography concepts such as salinity and temperature gradients.
  • Familiarity with the Coriolis effect and its impact on fluid dynamics.
  • Knowledge of surface and deep ocean currents and their driving forces.
  • Basic principles of heat transfer in oceanic systems.
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  • Research the Coriolis effect and its role in ocean current formation.
  • Study the impact of salinity and temperature on ocean circulation patterns.
  • Explore the differences between surface currents and deep ocean currents.
  • Investigate the effects of climate change on ocean current dynamics.
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Oceanographers, climate scientists, and educators seeking to deepen their understanding of ocean current mechanics and their implications for global climate systems.

h4tt3n
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Hello everyone, first post on this forum...

Recently I've been trying to understand how ocean currents work from a general perspective. While studying, an intrigueing question popped up in my mind, and I haven't been able to let it go unanswered. It is simply:


If the Earth was a completely smooth, ocean covered sphere (but otherwise unchanged), how would the ocean currents flow?


I think that answering this Q might help one to understand what makes all the world's real ocean currents tick. Any suggestion?

Cheers,

Michael
 
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h4tt3n said:
If the Earth was a completely smooth, ocean covered sphere (but otherwise unchanged), how would the ocean currents flow?
I don't think they would - I thought the main currents were driven by salinity differences as fresh water enters at the pole ( at least for the northern hemisphere )
 
Surface currents: from equator N & S (plus coriolis E) to higher latitudes; once heat loss by radiation exceeds that absorbed from solar radiation, the water sinks, then flows from the poles toward the equator (again, plus coriolis W).
 

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