Grand Challenges in Ocean and Climate Modelling - STFC's ...
Grand Challenges in Ocean and Climate Modelling - STFC's ...
Grand Challenges in Ocean and Climate Modelling - STFC's ...
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NEMO 1/4° global ocean model surface temperature<br />
Thus a global ocean model of order 1 km horizontal resolution would explicitly<br />
resolve a good part of the <strong>in</strong>ternal wave spectrum. The result<strong>in</strong>g mix<strong>in</strong>g could then<br />
be easily <strong>in</strong>cluded through (for example) a Richardson number dependent scheme.<br />
Improved parameterisations could also be developed for lower resolution models.<br />
This would be likely to cause a major change <strong>in</strong> the deep circulation patterns <strong>in</strong><br />
the global ocean, <strong>and</strong> <strong>in</strong> the upwell<strong>in</strong>g of the deep waters, <strong>and</strong> <strong>in</strong> the way <strong>in</strong> which<br />
the ocean circulation is ma<strong>in</strong>ta<strong>in</strong>ed. Such a model would therefore lead to major<br />
improvements <strong>in</strong> ocean <strong>and</strong> climate modell<strong>in</strong>g systems <strong>and</strong> predictions, <strong>and</strong> to<br />
our underst<strong>and</strong><strong>in</strong>g of how the ocean works.