Many combinations of salinity and temperature of seawater can produce the same density of seawater.
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Q2: The large ocean surface-current gyres centered on
Q3: Isothermal water is stable and does not
Q4: In an area where surface currents converge,
Q5: Increasing salinity increases density.
Q6: Usually temperature, salinity, and pressure distributions cause
Q7: Antarctic bottom water has a very narrow
Q8: The pycnocline of the oceans is usually
Q9: The pycnocline is an area where temperature
Q10: Wind blowing across the sea surface can
Q11: In the oceans the zone where density
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