The activity offers separate wind and density views. Arrows in the wind view show an ideal surface response, not a map of actual currents. In the parcel view, temperature and salinity offsets decide a qualitative density tendency relative to neighbouring water. The display does not calculate a complete seawater equation of state.
Water and oceans · Discover & try
What can move water across the ocean?
Reading level 3 of 5 · IndependentChange
Word help
Density
Mass per unit volume.
Surface current
Water movement near the ocean surface, often strongly affected by wind.
Overturning
Circulation connecting shallower and deeper water.
Watch · Try · Explain
See how it works
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Conceptual wind and relative-density views; not a map or numerical seawater-density calculation.
What to look for
- Compare the parcel with surrounding water.
- Change temperature without changing salinity.
- Distinguish wind-driven surface movement from sinking.
Explain what you noticed
Two nearby parcels have the same salinity and pressure. One cools while the other does not. What tendency fits ordinary seawater conditions?
Keep this idea: Wind drives much surface circulation; temperature and salinity help influence water density and deeper movement.
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Source material checked 2026-10-28. Explanations and activities by Nepedia. Source links do not imply endorsement.
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