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Grand Challenges in Ocean and Climate Modelling - STFC's ...

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Internal Wave Mix<strong>in</strong>g <strong>in</strong> the Deep <strong>Ocean</strong><br />

Internal waves are thought to<br />

provide an important mix<strong>in</strong>g mechanism<br />

for stirr<strong>in</strong>g the deep ocean <strong>and</strong> upwell<strong>in</strong>g<br />

the deep waters to nearer the surface.<br />

This is an important route whereby waters<br />

which have left the surface can “overturn”<br />

<strong>and</strong> once more return to the surface. The<br />

mix<strong>in</strong>g is therefore critical to ma<strong>in</strong>ta<strong>in</strong><strong>in</strong>g the<br />

large-scale circulation <strong>in</strong> the ocean.<br />

The figure (from theory) shows that <strong>in</strong>ternal<br />

tides <strong>and</strong> waves provide 0.9 TW of energy<br />

to the deep ocean, nearly half of the total<br />

required (the rema<strong>in</strong>der be<strong>in</strong>g provided by<br />

the w<strong>in</strong>d).<br />

From Munk & Wunsch (1998)

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