<p><strong>Fig 2.21.</strong> (<strong>A</strong>) Thermohaline circulation in the Mediterranean Sea is driven by high rates of evaporation. Salty dense water sinks and less dense water from the Atlantic ocean basin flows into the sea.</p>

Fig 2.21. (A) Thermohaline circulation in the Mediterranean Sea is driven by high rates of evaporation. Salty dense water sinks and less dense water from the Atlantic ocean basin flows into the sea.

Image by Byron Inouye